Text (very rough draft).

advertisement

1

9

10

7

8

5

6

3

4

11

12

13

14

15

1

2

Carbon and Nitrogen Accumulation in a 16-year Old Naturally

Regenerated Loblolly Pine Stand

P.R. Kapeluck*, W.D. Carroll, D.H. Van Lear, E.A. Mikhailova, C. J. Post, M. A. Schlautman and W.M. Post

P.R. Kapeluck, W.D. Carroll, D.H. Van Lear, E.A. Mikhailova, C.J. Post, Department of Forestry and Natural Resources, Clemson University, 261 Lehotsky Hall, Clemson, SC 29634-0317; M.A.

Schlautman, Department of Environmental Toxicology, Clemson University, Clemson, SC

29634-0317; W.M. Post, Environmental Sciences Division, Oak Ridge National Lab., Oak Ridge,

TN 37831-6422.

*Corresponding author (pkplck@clemson.edu).

2

16

17

Carbon and Nitrogen Accumulation in a 16-year Old Naturally Regenerated

Loblolly Pine Stand

18

19

ABSTRACT

20 Rationale: The effects of the whole-tree and stem-only harvests on plant biomass, plant/soil

21 carbon (C) and nitrogen (N) stocks of naturally regenerated loblolly pine ( Pinus taeda L.) grown

22 in the Southeastern U.S. are poorly understood.

23 Objectives or hypothesis: This study was conducted to determine whether different tree-

24 harvesting methods could be manipulated to maximize plant biomass, plant/soil C and N

25 sequestration in naturally regenerated loblolly stands.

26 Methods: The effects of the whole-tree and stem-only harvests on the plant biomass, plant/soil C

27 and N stocks were investigated at the naturally regenerated loblolly pine stand at Clemson

28 Experimental Forest in Clemson, SC, on an abandoned agricultural field with eroded Pacolet soils

29 (Typic Kanhapludults).

30 Results:

31 A study at 5 yr found the S harvest had 29% more accumulated above-ground phytomass (live

32 and dead biomass) and 29 and 15% more C and N, respectively, than the W harvest. The trend

33 was similar at 16 yr with S harvest phytomass, C, and N levels 20, 20, and 103 % greater than the

34 whole-tree harvest. More growth and larger stocks of C and N for the S harvest may be related to

35 the release of elements contained in the logging debris during decomposition, N-fixation in

36 decomposing logging debris, and the environment it created. However, there were no statistically

37 significant differences in soil C and N between harvest methods.

38 Conclusions:

3

39 INTRODUCTION

40 Temperate forest ecosystems have been identified as potentially important for sequestering

41 carbon from the atmosphere for long-term storage (Tans et al. 1990) and harvesting effects on

42 forest productivity have been a concern for decades. As long ago as 1923, Wiedeman attributed

43 second rotation declines in productivity of spruce stands in Germany, Norway, and Switzerland to

44 soil degradation caused by clearcutting. However, solid evidence of reduced growth after

45 repeated harvests is limited to relatively few studies (Rennie 1955; Bednall 1968; Gholz et al.

46 1984).

47 More recently, concern has been expressed about effects on soil organic matter and forest

48 productivity when harvesting removes nearly all aboveground biomass (Johnson and Todd 1998).

49 Powers (1989) and Van Cleve and Powers (1995) suggested that productivity is ultimately related

50 to the amount and kind of soil organic matter. Johnson (1992) and Fisher (1995), while agreeing

51 that there is an intuitive relationship between soil organic matter and forest growth, noted that

52 there is seldom a strong statistical relationship.

53 Mann et al. (1988) described conventional vs. whole-tree harvesting impacts on nutrient

54 pools and regeneration at a variety of sites in the United States. This paper characterizes

55 productivity of loblolly pine ( Pinus taeda L.) of the Clemson, SC site 16 yr after treatment. We

56 hypothesize that, on eroded Piedmont sites, removal of logging debris during whole-tree

57 harvesting would reduce productivity and C and N sequestration.

58 MATERIALS AND METHODS

59 The study was located on the Clemson University Experimental Forest in the upper Piedmont of

60 South Carolina. The sites were within a 12.4 ha loblolly pine plantation established in 1939 on a

61 severely eroded nutrient-depleted agricultural field. Soil is an eroded phase of the Pacolet fine

4

62 sandy loam, a typic thermic Kanhapludult, and well drained. The coarse textured brown surface

63 layer ranged from sandy loam to sandy clay loam and was underlain by red, firm clay loam and

64 clay. Most of the surface soil had been lost during a century of farming (Trimble 1974) which

65 caused its depth to vary widely and frequently exposed the subsoil. Erosion essentially ceased

66 after plantation establishment.

67 The plantation occupied a hillside with an average slope of 13 % and S-SW aspect.

68 Average diameter breast height (DBH) was 25.5 cm and average height of dominant and

69 codominant trees was 23.2 m. Site index was 24.4 m at age 50 yr. Thinning from below at ages

70 22 and 30 yr had increased the original 2 x 2-m spacing to about 5 x 5 m, leaving an average of

71 437 stems ha

-1

and 18.5 m

2

ha

-1 basal area. Annual precipitation averages 130 cm and is well

72 distributed throughout the year.

73 Two watersheds (<2.0 ha/ea) within the plantation, separated by a 200-m-wide uncut area,

74 were clearcut in the winter of 1979 – 80, one using stem-only harvesting and the other whole-tree

75 harvesting. The methods of Van Lear et al. (1984) and pre-harvest DBH values generated

76 estimates of biomass and N content of logging debris remaining on the S harvest (20 Mg ha

-1

). All

77 debris was removed from the W harvest. Natural regeneration of both watersheds was from seed

78 produced by the surrounding stand on seedbeds prepared prior to harvest with prescribed fire.

79 Prior to the 1979 – 80 harvests, a 100% inventory of the 41-yr-old plantation was completed,

80 including the two study watersheds, for estimates of stem density, DBH, and basal area. Nutrient

81 content of the forest floor and soil just after harvest were reported in Van Lear et al. (1983).

82 Forest floor C content was estimated as 50 % (Taylor et al. 1991, Maier et al. 2004, Katul 2005)

83 of ash-free biomass. Five year post-harvest estimates of pine and other vegetation density,

84 biomass, and nutrient content were reported in Cox and Van Lear (1985). Residual pine root

5

85 system biomass and nutrient content just-after-harvest was determined as in Kapeluck and Van

86 Lear (1995). Carbon content of residual root systems was estimated as 50 % of biomass

87 (citation).

88

89 A comparison of preharvest data for both treatments is shown in Table 1. While the S

90 harvest has 26% more stems than the W harvest, both treatments have fewer stems than the

91 plantation average, and basal area for the W harvest exceeds the conventional harvest and the

92 plantation average. Higher stem density may explain the lower DBH in the S harvest. Greater

93 pre-harvest biomass (33%) on the W harvest suggests it was the better quality site.

94 Treatment effects were examined using estimates made just prior to harvest of the 41-yr-

95 old stand, just after harvest, 5 yr after harvest, and 16 yr after harvest. Estimates included 1),

96 density, biomass and nutrient content of the preharvest pine stands, 2), pine biomass and nutrient

97 content just after harvest, 3), forest floor biomass and nutrient content just after harvest, and 4),

98 nutrient content of the upper 60 cm of mineral soil just after harvest. Estimates at five years post-

99 harvest included pine density, biomass, and nutrient content and that of competing vegetation.

100 Sixteen years post-harvest estimates included 1), above-ground pine density, biomass, and C and

101 N content, 2), forest floor biomass and C and N content, and 3), C and N content of the upper 60

102 cm of mineral soil.

103 Carbon mass was estimated as 50% of biomass ( Wood Energy Hanbook, Maier et al.

104 2004, Katul 2005). Forest floor and soil nutrient content just after harvest were reported in Van

105 Lear et al. (1983). Residual pine root biomass and nutrient content just after harvest was

106 estimated as in Kapeluck and Van Lear (1995).

6

107 Treatment effects on heights of the 16-yr-old regeneration were estimated from height-

108 pole measurements of 15 codominant and dominant trees from each treatment.

109 Aboveground biomass of 16-yr-old stands was estimated using equations developed from

110 16 trees representing the range of diameters present in the two treatments as in Van Lear et al.

111 (1984). These equations were applied to diameter-breast-high (1.4 m) of trees on three randomly

112 located 10 x 20 m plots/treatment. Each plot contained 20-30 pine trees. Necromass was

113 estimated the same way from 16 standing dead trees/treatment. Pine root biomass and nutrient

114 content of the 16-yr-old stand was estimated as in Kapeluck and Van Lear (1995). Foliage,

115 branch, bole, necromass, forest floor, and soil C and N of the 16-yr-old stands were determined on

116 a Perkin-Elmer 240C Analyzer.

117 Soil was sampled at 0-8, 8-30, and 30-60 cm depths in each plot from cores (2.5-cm dia)

118 taken at three points/plot/treatment. Soil mass excluded rock and pine root volume determined in

119 previous studies (Kapeluck and Van Lear 1995, Parker and Van Lear 1996). Concentrations were

120 multiplied by compartment mass to determine elemental content.

121

123

Height for the 16-yr-old regeneration were . Differences in phytomass components and

122 elemental concentrations were detected using t tests.

Equations were developed using SAS (1992).

124

125

126

RESULTS

An essential estimate needed to assess the effects of the two harvesting treatments was an

127 evaluation of comparative productivity of the two areas prior to treatment. Stem analysis of the

128 mature trees growing along the boundaries of each treatment provided one detail to answer this

129 question. Comparison of height/age growth patterns revealed that growth on the two treatments

7

130 were different during the 41 yr preceding treatment (Fig. 1). Although the average height growth

131 of the conventional harvest treatment was only 1.6 m less than the whole-tree harvest treatment

132 after 41 yr, the difference between regressions was significant (p = 0.001). More importantly, this

133 difference corresponds with the other pretreatment estimates which indicate that productivity of

134 the conventional harvest treatment was the lesser of the two treatments.

135 Table 2 compares mass and elemental content of residual pine biomass (above and

136 belowground), forest floor, and mineral soil for both treatments just after harvest operations were

137 completed. The totals found at the bottom of the table provide some explanation for the greater

138 preharvest productivity of the whole-tree harvest treatment area. Only overall biomass of the

139 conventional harvest treatment, which includes 20 Mg ha

-1

of residual crown biomass, is higher

140 (11.7%) than that of the whole-tree harvest treatment. For element content, the whole-tree harvest

141 treatment ranges from about 5 to 128% greater than the conventional harvest treatment. Among

142 the three compartments, differences between treatments for C, N, and P were greatest in the forest

143 floor. The 22% greater forest floor biomass of the whole-tree harvest area implies its greater

144 productivity and reflects its greater pretreatment foliage biomass. For K and Ca, differences

145 between treatments were greatest in mineral soil where the whole-tree harvest treatment contained

146 about twice the amount of the conventional harvest treatment. Forest floor differences between

147 treatments for K and Ca were also large, at 23 and 61%, respectively.

148

149

After the first growing season the whole-tree harvested treatment had more than twice the regeneration of the conventional harvest treatment with 82,000 and 33,000 stems ha

-1

,

150 respectively. At the end of the fifth growing season, regeneration density of the conventional

151 harvest and whole-tree harvest treatments had declined to nearly equal numbers, 23,000 and

152 20,500 stems ha

-1

, respectively. However, at the end of the fifth growing, total biomass of

8

153 herbaceous vegetation, hardwood sprouts, and pine saplings on the conventional harvest treatment

154 comprised about 29% more than that on the whole-tree harvest treatment (Table 3). Although

155 other species continued to be present in the stand their fraction of total plant biomass had declined

156 sharply during the previous five years as pine regeneration had rapidly become the dominant

157 vegetation. At that time pine biomass when averaged for both treatments made up about 78% of

158 total vegetation biomass. Because of high regeneration density crown closure was apparently

159 already underway on both treatments.

160 During the next 11 yr live pine density of the whole-tree harvest treatment continued its

161 more precipitous decline until at age 16 yr it contained about 35% fewer live stems (Table 4).

162 Standing dead stems on the conventional harvest treatment were also more numerous (17%) than

163 those on the whole-tree harvest treatment. Combined live and dead stems on the conventional

164 harvest treatment were about 38% more abundant than on the whole-tree harvest treatment.

165 Further attrition of live stems through self thinning during the years from 5 to 16

166 eliminated about 50% of the regeneration on the whole-tree harvest treatment in contrast to the

167 30% loss on the conventional harvest treatment. These comparisons suggest that the environment

168 of the whole-tree harvest treatment was considerably less favorable for seedling and sapling

169 survival. Although not significant, and perhaps unexpected, mean dbh of both live and dead

170 stems on the whole-tree harvest treatment are slightly larger than those of the conventional

171 harvest treatment (Table 4). This trend may result from the distribution of site resources among

172 fewer trees.

173 By age16 yr loblolly pine regeneration completely occupied the growing space on both

174 treatments which created a deeply shaded understory nearly free of other plants. Phytomass

175 accumulation after 16 yr were similar to those observed after 5 yr (Fig. 2), which continued the

9

176 trend of lower productivity on the whole-tree harvest treatment. Tree boles, the largest and only

177 component significantly different between treatments, were 35% greater on the conventional

178 harvest treatment. Boles comprised 60% and 68% of the total above-stump phytomass for the

179 whole-tree and conventional harvest treatments, respectively (Table 5).

180 As discussed, mortality rates were high during the 16 yr prior to these measurements

181 because of intense intraspecies competition as trees continued to differentiate into crown classes.

182 Standing necromass at age 16 yr was 10.9 Mg ha -1 for the whole-tree harvest treatment and 12.0

183 Mg ha

-1

for the conventional harvest treatment (Table 5). Most dead trees remained standing

184 because high stand densities on both treatment areas prevented their falling. When necromass

185

186 was combined with biomass, total aboveground loblolly pine phytomass was 19.6% more (141.4 vs. 118.2 Mg ha

-1

) for the conventional harvest treatment. In comparison, Wells et al.(1975)

187 reported 156.0 Mg ha -1 of aboveground biomass for a 16-yr-old loblolly pine plantation with

188 2,243 trees ha

-1

(approximately 1/7 and 1/5 the density of our stands) on an excellent site in the

189 North Carolina Piedmont.

190 Our stands are growing on eroded and nutrient deficient soil that often experiences

191 moisture deficits during the growing season (Myers et al. 1986). Extremely high seedling density

192 probably initiated intense competition for nutrients, water, light, and growing space during the

193 first growing season after the treatments were applied. Thus, treatment-induced stress may have

194 been reflected earlier in these dense stands than in more widely spaced plantations, especially on

195 poor quality sites. Since pine density remained extremely high throughout the study period the

196 magnitude of growth differences between treatments may have been amplified.

197 Although biomass productivity was about 20% greater on the conventional harvest

198 treatment, no differences between treatments could be detected in height/age growth patterns of

10

199 the regeneration during their 16 yr of growth (Fig. 3). Nor were differences found in the mean

200 stand heights of the treatments (Table 6).

201 A partial explanation for similar height/age growth patterns and stand height may be the

202 more rapid self thinning that occurred on the whole-tree harvest treatment. As previously

203 discussed, high stem density intensified competition for finite resources on both treatments. And,

204 although stem density had declined dramatically, especially on the whole-tree harvest treatment, it

205 remained very high for both treatments. The continued high density exerted the competitive

206 stimulation for height growth on both treatments, but, for the whole-tree harvest treatment, its

207 apparently more limited resources could be concentrated in fewer surviving trees. Thus,

208 comparable height growth was maintained. Smith (1986) postulated that on poorer sites, seasonal

209 moisture deficiencies or other soil factors limit production more at high stand densities than at

210 intermediate levels consistent with full or nearly full occupancy.

211 It is also possible that the codominant and dominant crown classes on the whole-tree

212 harvest treatment are primarily composed of trees growing near the old decomposing root systems

213 of the harvested 41-yr-old stand. How trees growing in these locations benefit will be discussed

214 later. On the whole-tree harvest treatment these trees would have a distinct competitive advantage

215 over other trees because the other trees would be subjected to the evident detrimental treatment

216 effects without the mitigation offered by the old root systems.

217 The greater aboveground mass on the conventional harvest treatment would be expected to

218 have correspondingly larger mass of coarse roots to maintain allometric relations between tops

219 and roots (Waring and Schlesinger 1985). Van Lear and Kapeluck (1995) demonstrated such a

220 relationship between tops and roots for mature loblolly pine on this site. Van Lear et al. (2000)

221 found that decomposing root systems of harvested loblolly pines provide a favorable medium for

11

222 fine root growth and support a high density of such roots. Sixteen-year-old loblolly pines tended

223 to be larger and grew at greater densities close to these decomposing root systems. We believe

224 that tops of trees on the conventionally harvested site, as they decomposed, provided similar

225 microsites of enhanced rooting potential, i.e., less resistance to root penetration, greater aeration,

226 higher nutrient concentrations, and higher moisture-holding capacity, than the surrounding

227 mineral soil. Better quality rooting habitat and increased rooting volume offered by the

228 decomposing wood of the tops on the conventionally harvested treatment may account for some

229 of the greater productivity.

230 Other potential benefits of logging slash included shading the 40 to 60% of the soil surface

231 that it covered. After harvesting much of the solar load formerly used for evapotranspiration

232 heats the air, forest floor, and soil (Geiger 1965). Evaporation from forest floor and soil increase,

233 but the most important effect is the increase of temperature extremes. High temperatures increase

234 the decomposition rate of the forest floor and on bare soil surface temperatures have been

235 recorded as high as 58 C and a 15-day average of 48 C at 0.6 cm depth (USDA 1951). High

236 temperatures like these inhibit both survival and growth of seedlings. High soil temperatures also

237 dessicate the surface soil and reduce it to a structureless mass.

238 Shading from the residual crowns would moderate surface temperatures, reduce

239 evapotranspiration, lower moisture stress, and help maintain the structural integrity of the friable

240 and nutrient rich surface soil. This would have benefitted the trees on the conventional harvest

241 treatment since soil moisture has a greater influence on root and top growth than any other soil

242 factor because it effects nutrient availability, uptake, and transport (Pritchett 1979). Slash would

243 also provide a mulching effect which aids root growth (Bilan 1968) while preventing increases in

244 soil strength because soil strength increases sharply as it dries which limits root growth (Zahner

12

245 1968). Also, the scattered crowns formed a tall (3m) barrier to horizontal air movement near the

246 ground which increases after harvesting (Hursh 1948). This barrier effectively shifts the

247 temperature, humidity, and wind movement boundary layer above the soil surface (May 1977)

248 which provides a diffusion barrier for moisture and shades the surface from direct insolation. The

249 result is improved conditions for survival and growth of trees and greater protection of the

250 desirable properties of forest soils such as low density, high porosity, and high infiltration rates

251 (Nutter and Douglass ______?).

252 The S - SW aspect of both treatments caused daily exposure to long periods of direct

253 insolation. Without logging slash the whole-tree harvest treatment’s environment was not

254 moderated by the benefits discussed above and moisture loss/stress was undoubtably greater. Tree

255 and root growth slows or ceases with water deficits through interference with photosynthesis,

256 nitrogen metabolism, salt absorption, translocation, and cell enlargement (Kramer 1969, Pritchett

257 1979). The absence of these moderating factors may also have contributed to the productivity

258 differences.

259

Need to add reference for boles as the last part of the tree to receive

260

carbohydrate

261 Based on differences in nutrient accumulation in phytomass, the growth differences

262 between the two treatments appears to be primarily nutritional. At age 5 yr, the regenerating plant

263 community on the conventional harvest treatment had accumulated 13-15% more N, P, K, and Ca

264 in aboveground biomass (Table 7), indicating that larger quantities of nutrients were absorbed

265

266 early. Nutrient accumulation in aboveground phytomass at age 5 yr was very high on both treatments, e.g., 156 and 136 kg ha

-1

N for the conventional and whole-tree harvest treatments,

267 respectively. The extremely high densities of pine saplings in these stands may have allowed

13

268 more complete capture of available elements and more rapid element accumulation in pine

269 phytomass in contrast to the far lower pine densities found in plantations. In addition, the woody,

270 more decay resistant qualities of pine tissue compared to the rapid turnover rate of herbaceous

271 plant tissue may have slowed the nutrient turnover rate in these natural stands compared to

272 plantations. This would follow from the greater dominance and early canopy closure by pine in

273 these natural stands compared to plantations. Nemeth (1973) reported a decrease in turnover rate

274 of ground litter to soil and a net decline of the net primary production of the lesser vegetation of

275 89% associated with canopy closure in pine plantations. As competition gradually reduced pine

276 density, the woody tissues of dead pines would have decomposed and released nutrients relatively

277 slowly.

278 The lower turnover rate of woody pine tissue may have also contributed to a tighter

279 nutrient cycle because pine root occupancy of the soil would have been consistently at or near

280 maximum because of constant high stand density. High stem density is concomitant with equal

281 numbers of root systems which would have produced a densely populated subsurface mat of

282 interwoven pine roots. This root mat would have been present almost continuously from the first

283 through the sixteenth growing season. Therefore, in these natural stands, pine roots would have

284 been more likely to absorb available elements and those released during detrital decay rather than

285 their being lost to leaching. However, element conservation may have been less effective on the

286 whole-tree harvest treatment because of its more rapid decline in stem density/root systems,

287 perhaps allowing greater leaching losses.

288 Aboveground phytomass on the conventional harvest treatment at age 16 yr contained

289 markedly greater quantities of nutrients. Nitrogen, P, K, and Ca were 2.0, 1.7, 1.2, and 1.4 times,

290 respectively, more than the whole-tree harvest treatment. Nitrogen content of the natural stand on

14

291 the conventional harvest treatment was much larger than values reported for similarly aged

292 plantations of southern pines, e.g., more than twice that of a 16-yr-old loblolly plantation on an

293 excellent site in the Piedmont of North Carolina (Wells et al. 1975) and 50% greater than that of a

294 fertilized 15-yr-old slash pine plantation in Florida (Pritchett and Smith 1974).

295 The large differences in nutrient accumulation by stands on the two treatments relates to

296 land-use history, as well as to effects of treatment on nutrient availability and uptake. Upper

297 Piedmont soils were depleted of nutrients and organic matter by a century of row cropping for

298 cotton, tobacco, and other crops prior to reforestation in the 1930s (Giddens 1957; Trimble 1974;

299 Van Lear and Kapeluck 1995). The absence of logging debris following whole-tree harvesting

300 may jeopardize productivity on sites with low levels of available N (Weetman and Webber 1972;

301 van den Driessche 1991). Nitrogen often limits growth on Piedmont sites, but responses to N

302 fertilization by Piedmont plantations are generally short lived (Van Lear 1980; Wells and Allen

303 1985; Jokela et al. 1991). Therefore, the slowly released N in logging debris may be important to

304 the productivity of these soils.

305

306

Estimates of elemental content of logging debris (Van Lear et al. 1984) were approximately 53, 5, 19, and 37 kg ha

-1

of N, P, K, and Ca, respectively (Table 8). About 50% of

307 the N and P in this debris is in relatively nutrient-rich and readily decomposable foliage. Some of

308 these nutrients would have been available for plant uptake during the regeneration period and

309 probably enhanced early growth on the conventional harvest treatment. In addition, the mulching

310 effect of the debris, which covered about 40 - 60% of the area (based on aerial photographs and

311 tree crown calculations), probably conserved soil moisture creating a more favorable rooting

312 environment during the regeneration period. As the woody portions of logging slash decomposed,

313 it probably became an enhanced medium for fine root growth much in the same manner that

15

314 decomposing root systems do (Van Lear et al. 2000). Enhanced root growth would have allowed

315 trees on the conventionally harvested treatment to absorb greater quantities of nutrients. Nitrogen,

316 P, and Ca in regrowth on the conventional harvest treatment diverged sharply from that of the

317 whole-tree harvest treatment between ages 5 to 16 yr (Fig. 4).

318 Phytomass nutrient differences between the two treatments (Table 9) were larger than

319 absolute quantities of nutrients in logging debris. Bole and branch components in the 16-yr-old

320 stand accounted for most of the unexpectedly large quantities of nutrients on the conventional

321 harvest treatment. Boles there contained 3.8, 2.5, 2.0, and 1.6 times more N, P, K, and Ca,

322 respectively, than those on the whole-tree harvest treatment, although bole mass was only 35%

323 greater on the conventional harvest treatment.

324 Differences in nutrient content of boles were a result of large differences in nutrient

325 concentrations, rather than in phytomass (Table 10). Nitrogen concentrations of boles from the

326 conventional harvest treatment were almost three times higher than those of the whole-tree

327 harvest treatment, while P concentrations were twice as high. There were significantly greater

328 concentrations of N, P, and K in branches (live and dead) of trees on the conventional harvest

329 treatment. Nitrogen concentrations in foliage from the two treatments did not differ. Bole

330 concentrations of N reported here for the conventional harvest treatment are higher than others

331 reported in the literature for pine plantations (Wells et al. 1975, Tew et al. 1984). We have no

332 reason to doubt the accuracy of our reported concentrations. As seen in Table 6, concentrations of

333 all elements in boles of trees in the conventional harvest treatment were higher and had small

334 standard errors. Other support for unbiased concentrations is that the elemental analysis was

335 performed at an independent lab and the sample vials were only identified by sequential numbers.

16

336 Reasons for higher concentrations of nutrients in phytomass on the conventional harvest

337 treatment have not been determined, although the literature suggests several processes may be

338 involved. The gradual decay of logging debris, acting on a burned seedbed, may have enhanced

339 nutrient supply and availability, which acted as a starter dose of fertilizer while stimulating N

2

340 fixation. Reported rates of N fixation by free-living diazotrophs and N-fixing plants (Richards

341 1964; Roskoski 1980; Stevenson 1986; Jurgensen et al. 1987; Perry et al. 1987) range from

342 relatively insignificant amounts to well over 150 kg ha -1 yr -1 . Nitrogen supply and availability

343 also may have been enhanced by termites (Lee and Wood 1971; Behnke 1977; Brian 1978),

344 which were observed in logging debris.

345 Large N accumulations in pines have been attributed to associative N

2

fixation in the

346 rhizospheres (Richards 1973; Bormann et al. 1993). Although evidence that associative N

2

347 fixation exists in pines is convincing, organisms and processes involved are not well understood.

348 However, the moderated environment under and around decomposing logging debris may favor

349 microflora, including beneficial rhizosphere organisms. In addition to associative fixation,

350 mycorrhizal fungi have the ability to obtain N from organic sources and pass it on to conifers.

351 They also increase P availability (Harley and Lewis 1969; van den Driesssche 1991). It has also

352 been postulated that the pine rhizosphere mineralizes some fraction of soil N and P (Voight 1965;

353 Fisher and Stone 1969), providing another source of nutrients. The greater root mass assumed the

354 conventional treatment would have more rhizosphere, thus greater nutrient uptake would be

355 expected.

356 Some or all of these soil processes were operating in both treatments but those in the

357 conventional harvest treatment were evidently enhanced by debris remaining on the site.

358 However, we suggest that the enhanced rooting value of the decomposing tops of harvested trees

17

359 is the most likely reason for the increased growth on the conventional harvest site. We believe

360 that decomposing tops provide a medium for enhanced fine root growth and root viability,

361 allowing greater nutrient uptake and accumulation in boles of trees on the conventional harvest

362 site. The network of decomposing tops scattered over the site essentially improved site fertility

363 (the ability of the site to supply nutrients) and thereby increased its productivity.

364 A summary of the status of the three ecosystem compartments 16 yr after the application

365 of treatments is shown in Table 11 in the same format as Table 2 for ease of comparison. Pine

366 phytomass on the conventional harvest treatment has exceeded pretreatment mass by 41% while

367 the whole-tree harvest treatment is 11% below pretreatment mass. Elemental accretion in pine

368 phytomass reflect the different rates of stand aggradation between treatments resulting in a

369 reversal in ranking of pine elemental capital. Swaps in forest floor mass ranking correspond to

370 the trends exhibited by the regenerating stands. Forest floor mass increased by16% for the

371 conventional harvest treatment during the past 16 yr while the whole-tree harvest treatment lost

372 14%. Similarly the ranking of elemental content of the forest floors also reversed except for

373 Ca.Ranking changes in mineral soil elemental content occurred only for C and P. The 29% loss in

374 C content for the whole-tree harvest treatment during the 16 yr since treatment may be related to

375 its lost productivity and therefore lower C inputs while detrital catabolic rates remained constant.

376 Nitrogen levels have remained about the same and any soil losses could have moved into pine

377 biomass or forest floor. Soil P on the conventional harvest treatment has increased dramatically

378 (296%) while the whole-tree harvest treatment increased a comparatively modest 37%. Potassium

379 in soil declined 69 and 62% for the conventional and whole-tree harvest treatments, respectively,

380 perhaps relocated in pine biomass. Calcium levels in soil have increased (55%) for the

18

381 conventional harvest treatment and decreased (-9%) for the whole-tree harvest treatment.

382 Calcium depletion citations/discussion.

383 Sums of elemental capital of the three ecosystem compartments estimated at the time of

384 treatment and16 yr later are compared in Table 12. This summary is perhaps the most dramatic

385 indication of the long-term treatment effects. During the 16 post-treatment years the conventional

386 harvest treatment has increased its combined elemental capital in all five elements from 16 to

387 197%. If C is included, the average elemental gain is 92%. For elements N, P, K, and Ca alone

388 the average increase is 34%. As a C sink, the conventional harvest treatment has nearly doubled

389 the quantity present in logging slash, forest floor, roots, and mineral soil on the site just after

390 harvest.

391 In marked contrast, changes in elemental capital for the whole-tree harvest treatment

392 consisted of more modest gains of 2 to 53 % combined with a 20% loss of K and a 0.2% loss of

393 Ca. If C is included, the average elemental gain is 50% and for N, P, K, and Ca alone the average

394 increase is only 2%. As a C sink, the whole-tree harvest treatment has increased its content by

395 53% since treatment. This quantity represents about 60% of the rate of C sequestration of the

396 conventional harvest treatment.

397 Although statistics are not possible for comparisons of the summary data in Table 12, the

398 magnitude of the differences in treatments strongly implies the detrimental effects of whole-tree

399 harvesting. Sixteen years after the treatments were applied the ranking of the original qualities of

400 the two sites has essentially been reversed.

401 If organic matter and associated nutrients from decomposing logging slash are stored

402 preferentially in old root channels and new roots disproportionately use them, should we not look

403 there to detect relationships between soil C and productivity? Old root channels are dynamic

19

404 elements of forest soils, beginning as dying roots and proceeding through various stages of decay.

405 They are hollowed from the inside by termites and other organisms, leaving the outside of the

406 opening intact. Gradually, the hollow core of the large taproot and major laterals are filled with

407 mineral and organic matter by soil fauna activity, as well as with roots from the developing plant

408 community. In time, perhaps decades or centuries, the old root channels blend into the soil

409 matrix.

410 The root distribution of young loblolly pine trees suggests that we sample more intensively

411 in or near decomposing root systems of harvested trees if we wish to detect relationships between

412 organic matter and productivity. Deposition of decaying logging debris in old root channels by

413 soil fauna and heavy utilization of these root channels by roots of the developing stand may

414 account for the relatively long-term positive growth response on the conventionally harvested

415 area.

416

417

Although soil carbon levels were not significantly different based on our random sampling design it is possible that some of the 10 Mg ha

-1

C contained in the logging slash could be

418 detected if the points where the slash decomposed were sampled specifically. The greatest

419 quantity of carbon in logging slash is found in the larger woody portions. The woody parts of

420 each crown occupy only a small fraction of the soil surface and it is unlikely that their residual

421 carbon would diffuse very far in surrounding soil. Therefore, to detect carbon from decomposed

422 logging slash, requires a stratified scheme that samples points where logging slash decomposed as

423 well as the rest of the stand. Otherwise, the probability of sampling these points would be low

424 and the greater carbon content of these samples would be masked by the predominantly lower

425 content of samples taken elsewhere in the stand.

426

20

427 DISCUSSION

428

429

430

SUMMARY AND CONCLUSIONS

Whole-tree harvesting should be carefully scrutinized before applying the practice on

431 marginal sites in the Piedmont. The naturally regenerated loblolly pine on the conventional

432 treatment grew significantly faster (20% more phytomass after 16 yr) than the that on the whole-

433 tree treatment. The major portion of this growth differential is attributed to greater nutrient

434 availability and uptake on the conventional treatment.

435 Although not found in this study, perhaps differences in height/age growth patterns will

436 emerge in later years as the stands mature and internal transfer and recycling elements become the

437 more dominant metabolic strategy. This may result as the more limited nutrient capital is diluted

438 in accumulating biomass and concentrations fall to levels which limit metabolic functions and

439 height growth.

440 This study indicates that nutrients released gradually during natural decomposition of

441 logging debris, in combination with other debris-mediated mechanisms which allow additional

442 nutrients to become available, produce a long-term sustained growth response in dense natural

443 pine stands on poor sites. This long-term increase in nutrient supply and availability, as indexed

444 by nutrient uptake, is critical to loblolly pine growth on poor sites when growth rates are

445 accelerating. Results from this study suggest that leaving logging debris in place is extremely

446 important to sustaining productivity on marginal sites.

447 The marked deterioration of the whole-tree harvested treatment from pretreatment levels

448 may be linked to the initial degraded quality of the old field site. With only 41 yr under loblolly

449 pine forest, the reclamation of pre-agricultural site quality would have only just begun. The hard

21

450 won accumulation of elements and organic matter appear to have been in a fragile and tenuous

451 state. The conservative conventional harvest used here, with crowns left where they fell (not

452 piled), allowed better retention and continuation of the capacity added to these poor quality sites

453 by the 41-yr-old loblolly pine plantation. The continued improvement of the conventional harvest

454 treatment further suggests that, with conservative management that duplicates the method used

455 here, successive rotations of loblolly pine will continue to improve productivity. Thus, site index

456 in the future may rise incrementally with each new stand.

457 As was expected the relationship between soil carbon and productivity was poor in this

458 study. Perhaps this is because we do not completely understand the complex pathways of detritus

459 decomposition and because it is difficult to separate effects of C on productivity from those of

460 associated nutrients. However, relationships between forest productivity and soil carbon may

461 become clearer if soils are examined in those areas where biological activity is greatest, i.e., in

462 and adjacent to old root channels and other points where organic matter is concentrated.

463

464

ACKNOWLEDGMENTS

This study was funded by the National Council of the Paper Industry on Air and Stream

465 Improvement, Inc. and McIntire-Stennis. Funding secured by Dale W. Johnson of the Desert

466 Research Institute was instrumental to the initial and latter phases of this study.

467

22

468 REFERENCES

469 Alban, D.H., and Perala, J. 1993. Decomposition of aspen, spruce, and pine boles on two sites in

470

471

Minnesota. Can. J. For. Res. 23 :1744-1749.

Behnke, F.L. 1977. A Natural History of Termites. Charles Scribner’s Sons, New York.

472 Bengtsson, J., and Wikstrom, F. 1993. Effects of whole-tree harvesting on the amount of soil

473 carbon: model results. N. Zeal. J. For. Res. 23 :380-389.

474 Bormann, B.T., Bormann, F.H., Bowden, W.B., Pierce, R.S., Hamburg, S.P., Wang, W., Synder,

475

476

M.C., Li, C.Y., and Ingersoll, R.C. 1993. Rapid N

2

fixation in pines, alder, and locust: evidence from the sandbox ecosystem study. Ecol. 74 : 583-598.

477 Bednall, B.H. 1968. The problem of lower volumes associated with second rotations in Pinus

478

479 radiata plantations in south Australia. In Proc. Ninth British Commonwealth For. Conf.

New Delhi. pp. 3-12.

480 Bilan, M.V. 1968. Effects of physical soil environment on growth and development of root

481 systems in southern pines. In Forest Fertilization - theory and practice. Tennessee Valley

482

484

Authority, Knoxville. pp. 15-19.

483 Brian, M.V. 1978. Production Ecology of Ants and Termites. International Biological

Programme 13. Cambridge University Press. New York.

485 Carlyle, J.C. 1993. Organic carbon in sandy soils: properties, processes, and the impact of forest

486 management. N. Zeal. J. For. Res. 23 :390-402.

487 Cox, S.K., and Van Lear, D.H. 1985. Biomass and nutrient accretion on Piedmont sites

488

489 following clearcutting and natural regeneration of loblolly pine. In Proc. Third South.

Silvicultural Res. Conf., Atlanta, Ga. Nov. 7-8, 1984. Gen. Tech. Rep. SO-54. New

490 Orleans, LA. USDA Forest Service, Southern Forest Experiment Station. pp. 501-506.

23

491 Fisher, R.E. 1995. Soil organic matter: Clue or conundrum? In Carbon Forms and Functions in

492 forest Soils. Edited by W. W. McFee and J. M. Kelly. Soil Sci. Soc. Am., Madison, WI.

493 pp. 1-11.

494 Fisher, R.F., and Stone, E.L. 1969. Increased availability of nitrogen and phosphorus in the root

495

497 zone of conifers. Soil Sci. Soc. Am. 33 :955-961.

496 Gholz, H., Fisher, R., and Pritchett, W. 1984. Nutrient dynamics in slash pine ecosystems. Ecol.

66 :647-659.

498 Giddens, J. 1957. Rate of loss of carbon from Georgia soils. Soil Sci. Soc. Am. Proc. 21 :513-

499 515.

500 Harely, J.L., and Lewis, D.H. 1969. The physiology of ectotrophic mycorrhyza. In Advances in

501

502

Microbial Physiology, Vol. 3. Edited by A.H. Rose and J.F. Wilkinson. Academic Press,

New York.

503 Husch, B., Miller, C.I., and Beers, T.W. 1982. Forest Mensuration. John Wiley & Sons, New

504 York. 402 p.

505 Johnson, D.W. 1992. The effects of forest management on soil carbon storage. Water, Air, and

506 Soil Pollution 64 :83-120.

507 Johnson, D.W. 1995. Role of carbon in the cycling of other nutrients in forested ecosystems. In

508

509

Carbon Forms and Functions in Forest Soils. Edited by W.W. McFee and J.M. Kelly.

Soil Sci. Soc. Am., Madison, WI. pp. 299-329.

510 Johnson, D.W., and Todd, Jr., D.E. 1998. Effects of harvesting intensity on forest productivity

511

512 and soil carbon storage in a mixed oak forest. In Management of carbon sequestration in soil. Edited by R. Lal, J. M. Kimble, R. F. Follet, and B. A. Stewart. CRC Press, New

513 York, NY. pp. 351-363.

24

514 Jokela, E.J., Allen, H.L., and McFee, W.W. 1991. Fertilization of southern pines at

515 establishment. In Forest Regeneration Manual. Edited by M.L. Duryea and P.M.

516 Dougherty. Kluwer Academic Publishers. Boston, MA. pp. 263-280.

517 Jurgensen, M.F., Larsen, M.J., Graham, R.T., and Harvey, A.E. 1987. Nitrogen fixation in

518

519 woody residue of northern Rocky Mountain conifer forests. Can. J. For. Res. 17 :1283-

1288.

520 Kapeluck, P.R. and Van Lear, D.H. 1995. A technique for estimating below-stump biomass of

521 mature loblolly pine plantations. Can. J. For. Res. 25:355-360.

522 Kramer, P.J. 1969. Plant and Soil Water Relationships: A Modern Synthesis. McGraw-Hill Book

523 Co., New York. 482 p.

524 Lee, K.E., and Wood, T.G. 1971. Termites and Soils. Academic Press. New York.

525 Mann, L.K., Johnson, D.W., West, D.C., Cole, D.W., and others. 1988. Effects of whole-tree and

526

527

531

532 stem-only clearcutting on postharvest hydrologic losses, nutrient capital, and regrowth.

For. Sci. 34:412-428.

528 Moore, B.R., Boone, D., Hobbie, J.E., Houghton, R.A., Melillo, J.M., Petersen, B.R., Shaver,

529

530

G.R., Vorosmarty, C.J., and Woodwell, G.M. 1981. A simple model for analysis of the role of terrestrial ecosystems in the global carbon budget. In Carbon cycle modelling.

Edited by B. Bolin. SCOPE Rep. 16, John Wiley & Sons, Chichester, England. pp. 365-

386.

533 Myers, R. K., Zahner, R., and Jones, S.M. 1986. Forest Habitat Regions of South Carolina from

534 Landsat Imagery. Clemson University Dept. of Forestry, For. Res. Series 42.

535 Nemeth, J.C. 1973. Dry matter production in young loblolly (Pinus taeda L.) and slash pine

536 (Pinus elliotti Englm.) plantations. Ecological Monographs 43(1):21-41.

25

537 Nutter, W.L. and Douglass, J.E. 1978. Consequences of harvesting and site preparation in the

538 Piedmont. In Proceedings: A symposium on principles of maintaining productivity on

539

540 prepared sites. Edited by T. Tippin. March 21-22, 1978. Mississippi State Univ.,

Mississippi State, MS. pp.65-72

541 Parker, M.M., and Van Lear, D.H. 1996. Soil heterogeneity and root distribution of mature

542 loblolly pine stands in Piedmont soils. Soil Sci. Soc. Am. Jour. 60 :1920-1925.

543 Perry, D.A., Choquette, C., and Schroeder, P. 1987. Nitrogen dynamics in conifer-dominated

544 forests with and without hardwoods. Can. J. For. Res. 17 :1434-1441.

545 Powers, R.F. 1989. Maintaining long-term forest productivity in the Pacific Northwest:

546

547

Defining the Issues. In Maintaining the long-term productivity of Pacific Northwest forest ecosystems. Edited by D.A. Perry et al. Timber Press., Portland, OR. pp. 3-16.

548 Pritchett, W.L., and Smith, W.H. 1974. Management of wet savanna soils for pine production.

549 Fla. Agr. Exp. Tech. Bull. 762.

550 Rennie, P.J. 1955. The uptake of nutrients by mature forest growth. Plant Soil 7 :49-95.

551 Richards, B.N. 1964. Fixation of atmospheric N in coniferous forests. Aust. For. 28 :68-74.

552 Richards, B.N. 1973. Nitrogen fixation in the rhizosphere in conifers. Soil Biol. Biochem. 5 :149-

553 152.

554 Roskoski, J.P. 1980. Nitrogen fixation in hardwood forests of the northeastern United States.

555

556

Plant Soil 54 :33-44.

SAS Institute. 1992. SAS User’s Guide. SAS Institute, Inc., Cary, NC.

557 Smith, D.M. 1986. The Practice of Silviculture. John Wiley & Sons, New York. 527 p.

558 Stevenson, F.J.H. 1986. Cycles of soil. John Wiley & Sons, New York.

559

26

560 Taylor, et al. 1991. Four Rocky Mountain Coniferous Forests. Canadian Journal of Botany

561 Tans, P.P., Fung, I.Y., and Takahashi, T. 1990. Observationa constraints on the global

562 atmospheric CO

2

budget. Science (Washington, D.C.), 247: 1431 – 1438.

563 Trimble, S.W. 1974. Man-induced soil erosion on the Southern Piedmont - 1700-1970. Soil

564

566

Conservation Society of America, Ankenny, IA.

565 Van Cleve, K., and Powers, R.F. 1995. Soil carbon, soil formation, and ecosystem development.

In Carbon Forms and Functions in Forest Soils. Edited by W.W. McFee and J.M. Kelly.

567 Soil Sci. Soc. Am., Madison, WI. pp. 155-200.

568 van den Driessche, R. 1991. Mineral nutrition of conifer seedlings. CRC Press. Boston.

569 Van Lear, D.H. 1980. Effects of nitrogen, phosphorus, and lime on the forest floor and growth of

570 pole-size loblolly pine. Soil Sci. Soc. Am. J.

44 :838-841.

571 Van Lear, D.H., Swank, W.T., Douglass, J.E., and Waide, J.B. 1983. Forest management

572

573 practices and the nutrient status of a loblolly pine plantation. p. 252-258. IUFRO

Symposium on forest site and continuous productivity. USFS Pacific NW Range Expt.

574

576

Sta. Seattle, Washington.

575 Van Lear, D.H., Waide, J.B., and Teuke, M.J. 1984. Biomass and nutrient content of a 41-yearold loblolly pine ( Pinus taeda L.) plantation on a poor site in South Carolina. For. Sci.

577 30 :395-404.

578 Van Lear, D.H., and Kapeluck, P.R. 1995. Above- and below-stump biomass and nutrient

579

581 content of a mature loblolly pine plantation. Can. J. For. Res. 25 :361-367.

580 Van Lear, D.H., Kapeluck, P.R., Parker, M.M. 1995. Distribution of carbon in a Piedmont soil as affected by loblolly pine management. In Carbon Forms and Functions in Forest Soils.

582 Edited by J.M. Kelly and W.M. McFee. Soil Sci. Soc. Am., Madison, WI. pp. 489-501.

27

583 Van Lear, D.H., Kapeluck, P.R., and Carroll, W.D. 2000. Productivity of loblolly pine as

584 affected by decomposing root systems. Forest Ecology and Management __:1-9.

585 Voight, G.K. 1965. Nitrogen recovery from decomposing tree leaf tissue and forest humus. Soil

586 Sci. Soc. Am. Proc. 29 :756-759.

587 Waring, R.H., and Schlesinger, W.H. 1985. Forest Ecosystems - Concepts and Management.

588 Academic Press, Inc. New York.

589 Weetman, G.L., and Webber, B. 1972. The influence of wood harvesting on the nutrient status of

590 two spruce stands. Can. J. For. Res. 2 :351-369.

591 Weideman, E. 1923. Zuwacksruckgang und Wuchstockingen der Fichte in den mittleren und den

592

594 unteren Hohenlagen der Sachsischen Staatsforsten. Tharandt. (Transl. 302) USDA.

593 Wells, C.G., Jorgensen, J.R., and Burnette, C.E. 1975. Biomass and mineral elements in a thinned loblolly pine plantation at age 16. USDA Forest Service Res. Pap. SE-126.

595 Southeast. For. Exp. Stn., Asheville, NC.

596 Wells, C.G., and Allen, H.L. 1985. When and where to apply fertilizer. A loblolly pine

597

598 management guide. USDA Forest Serv., Southeast. Forest Exp. Sta., Ashevillle, N.C.

Gen. Tech. Rep. SE-36.

599 Zahner, R. 1968. Water deficits and growth of trees. In Water Deficits and Plant Growth. Vol. 2.

Academic Press, Inc., New York. pp. 191-254. 600

601

602

28

603 Table 1. Preharvest characteristics of the 41-yr-old loblolly pine for the conventional harvest

604 treatment and whole-tree harvest treatment and plantation.

605

606

607

608

609

610

611

612

613

614

617

618

Treatment Stem Frequency DBH Basal Area Aboveground Biomass

(stems ha

-1

) (cm) (m

2

ha

-1

) (Mg ha

-1

)

Conventional 399 21.7 (0.407)

17.1 100.0

Whole-tree 316 29.0 (0.331) 21.7 133.2

Plantation 437 25.5 18.5 109.6

Standard errors.

619

29

629

630

631

632

633

634

635

636

637

638

639

640

641

642

643

644

620

621

622

623

624

625

626

627

628

Table 2. Comparison of ecosystem components of the conventional (C) and the whole- tree harvest treatment (W) just after harvest of the 41-year-old loblolly pine stand.

________________________________________________________________________

Treatment Component Biomass C N P K Ca

(Mg ha -1 )

(kg ha

-1

)

C Pine 44.4

22,420 95.4 10.4 47.2 71.4

W Pine 33.3



16,651 55.7 6.9 38.1 45.2

C Forest Floor 16.9 8,441 132.3 12.7 17.5 102.5

W Forest Floor 21.6 10,246 176.1 17.2 21.6 164.8

C Mineral Soil — 42,338  2,115.3 12.6 109.0 501.0

W Mineral Soil — 49,916 2,333.0 16.7 213.0 1332.0

________________________________________________________________________

Totals C 61.3 73,199 2,343.0 35.7 173.7 674.9

W 54.9 76,813 2,564.8 40.8 272.7 1,542.0

________________________________________________________________________

Includes residual crowns and root systems.



Includes only residual root systems.

 Soil values represent the upper 60 cm.

30

653

654

655

656

657

658

645

646

647

648

649

650

651

652

Table 3. Biomass and nutrient accretion in regrowth 5 years after stem-only (S) and whole-tree (W) harvest of mature loblolly pine in the Piedmont of South Carolina.

________________________________________________________________________

Treatment Biomass C N P K Ca

(Mg ha

-1

) (kg ha

-1

)

S 20.8 10,388

156.3 14.3 76.6 74.6

W 16.1 8,033 136.1 12.4 67.9 82.8

________________________________________________________________________

Carbon quantities are 50% of biomass values.

31

671

672

673

674

675

676

659

660

661

662

663

664

665

666

667

668

669

670

Table 4. Frequency and dbh for live and dead loblolly pine natural regeneration on stem-only and whole-tree harvest treatments in the Piedmont of South Carolina.

_______________________________________________________________________

Live Stem Dead Stem

Treatment Frequency DBH Frequency DBH

(No. ha

-1

) (cm) (No. ha

-1

) (cm)

________________________________________________________________________

Stem-only 15,954 5.21 (0.083)

10,451 1.80 (0.031)

Whole-tree 10,380 6.34 (0.105) 8,928 2.03 (0.034)

________________________________________________________________________

Numbers in parentheses are standard errors.

32

677

678

679

680

681

682

683

684

685

686

687

688

689

690

691

692

693

694

695

696

697

698

Table 5. Phytomass (biomass plus necromass) of naturally regenerated 16-year-old loblolly pine stands in the Piedmont of South Carolina following whole-tree and stem-only harvesting.

________________________________________________________________________

Tree

Component

Stem-only _

(Mg ha

-1

) (%)

Whole-Tree __

(Mg ha

-1

) (%)

________________________________________________________________________

Foliage

Dead branches

9.9a

*

10.8a

7.0

7.7

10.7a

11.4a

9.0

9.6

Live branches

Boles

Necromass

12.4a

96.3a

12.0a

8.8

68.1

8.4

13.9a

71.3b

10.9a

11.8

60.3

9.2

________________________________________________________________________

Total 141.4a 100.0 118.2b 100.0

________________________________________________________________________

Note:

*

Means within a row followed by different letters are significantly different at the 95% confidence level.

33

708

709

710

711

712

713

714

699

700

701

702

703

704

705

706

707

Table 6. Mean heights of 16-yr-old natural regeneration following conventional and whole-tree harvests in the Piedmont of South Carolina.

________________________________________________________________________

Treatment n Height

(m)

________________________________________________________________________

Conventional 15 9.82 (1.35)

a

Whole-tree 15 9.65 (1.40) a

________________________________________________________________________

Numbers in parentheses are standard errors.

Heights followed by the same letter are not significantly different at the 95% confidence level.

34

715

716

717

718

719

720

721

722

723

724

725

726

727

728

729

730

731

732

733

734

735

736

737

Table 7. Phytomass and nutrient content of aboveground regrowth 5 and 16 yr after whole-tree and conventional harvest of a mature loblolly pine plantation.

______________________________________________________________________________

Treatment Phytomass Nutrient

N P K Ca

____________(Mg ha

-1

)_______________________(kg ha

-1

)_____________________________

5th Year

136.1 12.4 68.0 82.8 Whole-tree 16.1

Conventional 20.8 156.3 14.3 76.6 74.6

Whole-tree 118.2

16th-Year

255.6 20.0 98.9 195.4

Conventional 141.4 519.2 33.7 118.1 267.8

______________________________________________________________________________

35

746

747

748

749

750

751

752

753

754

755

756

738

739

740

741

742

743

744

745

Table 8. Phytomass and nutrient content of logging debris following conventional harvest of mature loblolly pine plantations in the Upper Piedmont of South Carolina.

______________________________________________________________________________

Component Phytomass Nutrient________________

N P K Ca

___________________(Mg ha

-1

)__________________________ (kg ha

-1

)__________________

Stemwood

Stembark

4.2

0.4

2.7

0.7

0.2

0.1

1.8

0.2

3.3

0.7

Branches 12.7 23.8 2.3 10.8 28.3

Foliage 2.5 26.4 2.6 5.8 5.2

______________________________________________________________________________

Total 19.8 53.6 5.2 18.6 37.5

______________________________________________________________________________

36

776

777

778

779

780

781

782

783

784

785

786

787

766

767

768

769

770

771

772

773

774

775

757

758

759

760

761

762

763

764

765

788

789

790

Table 9. Phytomass and associated nutrient content for 16-year-old naturally regenerated loblolly pine in the Piedmont of South Carolina following conventional and whole-tree harvests.

______________________________________________________________________________

Component Phytomass Conventional

(Mg ha

-1

) C N P K Ca__

_____________________________________________(kg ha

-1

)_________________________

Foliage 9.9

Dead Branch 10.8

Live Branch 12.4

5.0

90.3 9.9 37.7 26.4

5.4 51.6 2.2 4.3 30.3

6.2 54.6 4.6 19.9 27.9

Boles 96.3 48.2 300.2 14.5 53.9 153.6

Necromass 12.0 6.0 22.5 2.5 2.3 29.6

Roots 35.4 17.7

59.1 7.4 40.4 48.0

Total 176.8 88.5 578.3 41.1 158.5 315.8

------------------------------------------------------------------------------------------------------------------

Component Phytomass

(Mg ha

-1

) C N

Whole-Tree

P K Ca___

_____________________________________________(kg ha

-1

)__________________________

Foliage 10.7

Dead Branch 11.4

Live Branch 13.9

Boles 71.3

5.4 98.0

5.7 24.8

7.0 32.1

35.7 79.5

9.0

1.1

2.8

5.8

52.8

0.8

15.8

27.4

28.4

25.0

26.9

93.5

Necromass 10.9 5.5 21.2 1.3 2.1 21.6

Roots 29.6 14.8 49.1 6.1 33.8 40.1

Total 147.8 74.1 304.7 26.1 132.7 235.5

______________________________________________________________________________

Carbon values for all components represent 50% of phytomass.

Element content of roots from Van Lear and Kapeluck (1995).

37

812

813

814

815

816

817

818

819

820

805

806

807

808

809

810

811

791

792

793

794

795

796

797

798

799

800

801

802

803

804

Table 10. Concentration means (n=16) of tree components from naturally regenerated 16-yr-old loblolly pine in the Upper Piedmont of South Carolina following conventional (C) and whole- tree (W) harvests.

______________________________________________________________________________

Tree

Component Trt. N P K Ca

______________________________________________________________________________

Bole

Bole

C .312a

*

(.026)

#

.015a (.002) .056a (.003)

W .112b (.010) .008b (.001) .038b (.006)

.16a (.032)

.13a (.015)

Live Brch.

Live Brch.

C

W

.440a (.034) .037a (.003) .160a (.014)

.230b (.017) .020b (.002) .114a (.015)

.23a (.026)

.19a (.009)

Dead Brch.

Dead Brch.

Foliage

C

W

.478a (.037) .021a (.002) .040a (.004)

.218b (.024) .010b (.001) .007b (.003)

.28a (.021)

.22b (.017)

C .912a (.014) .100a (.002) .380b (.026) .27a (.025)

Foliage W .916a (.021) .084b (.003) .494a (.029) .27a (.014)

______________________________________________________________________________

Note:

*

Means of each component followed by different letters are significantly different at the

95% confidence level.

#

Standard errors.

38

829

830

831

832

833

834

835

836

837

838

839

840

841

821

822

823

824

825

826

827

828

842

843

844

Table 11. Comparison of ecosystem components of the conventional (C) and whole-tree (W) harvest treatments 16 years after harvest of the 41-year-old stand.

______________________________________________________________________________

Treatment Component Biomass C N P K Ca

(Mg ha

-1

) ________________(kg ha

-1

)______________________

C Pine 176.8

88,375 578.3 41.1 158.5 315.8

W Pine 147.8 73,875 305.0 26.1 132.7 235.5

C Forest Floor 19.7 10,835 250.6 15.1 9.7 69.0

W Forest Floor 18.6 8,234 187.7 9.4 5.5 84.7

C Mineral Soil — 43,192

2,028.1 50.0 33.4 774.4

W Mineral Soil — 35,299 2,121.8 22.9 80.4 1,218.7

______________________________________________________________________________

Totals C 196.5 142,402 2,857.0 106.2 201.6 1,159.2

W 166.4 117,408 2,614.5 58.4 218.6 1,538.9

______________________________________________________________________________

Pine values include above and belowground biomass.

Soil values represent the upper 60 cm.

39

853

854

855

856

857

858

859

860

861

862

863

864

845

846

847

848

849

850

851

852

Table 12. Consolidated elemental capital of the conventional (C) and whole-tree (W) harvest treatment just after harvest of the 41-year-old stand and 16 years later.

______________________________________________________________________________

Treatment Sampling Date C N P K Ca

___________________(kg ha

-1

)_______________________

C 1980 73,199 2,343.0 35.7 173.7 674.9

C 1995 142,402 2,857.0 106.2 201.6 1,159.2

______________________________________________________________________________

Difference 69,203 514.0 70.5 27.9 484.3

W 1980 76,813 2,564.8 40.8 272.7 1,542.0

W 1995 117,408 2,614.5 58.4 218.6 1,538.9

______________________________________________________________________________

Difference 40,595 49.7 17.6 - 54.1 - 3.1

40

873

874

875

876

877

878

879

880

881

882

883

884

865

866

867

868

869

870

871

872

Table 13. Carbon content of the mineral soil in a 16-year-old naturally regenerated loblolly pine stand in the Piedmont of South Carolina following conventional and whole-tree harvesting.

______________________________________________________________________________

Depth

(cm)

Conventional Harvest

(Mg ha

-1

) (%)

Whole-tree Harvest

(Mg ha

-1

) (%)

______________________________________________________________________________

0-8

8-34

10.9a

*

20.0a

25

46

9.0a

16.4a

26

46

34-60 12.3a 29 9.8a 28

______________________________________________________________________________

Total 43.2 100 35.2 100

______________________________________________________________________________

Note:

*

Means within rows followed by different letters are significantly different at the 95% confidence level.

Download