EFFECTS OF WATERSHED RESTORATION ON WATER QUALITY AND QUANTITY OF KAPTAI LAKE IN BANGLADESH Laskar Muqsudur Rahman, PhD Conservator of Forests FOREST DEPARTMENT , BANGLADESH Forest types of Bangladesh Forest Types Unclassified State Forests Hill Forests Mangrove Forests Village Forests Coastal Afforestation Inland Sal Forests TOTAL million ha % 0.73 5.08 0.67 4.65 0.60 4.09 0.27 1.83 0.18 1.24 0.12 0.83 2.57 17.72 Forest Types of Bangladesh Unclassified State Forests 5.08% Hill Forests 4.65% Forest Types of Bangladesh Mangrove Forests 4.09% Coastal afforestation 1.24% (Mangrove) Forest Types of Bangladesh Sal Forests 0.83% (Shorea robusta) Village Forests 1.83% ? Forest Types of Bangladesh SOCIAL FORESTRY (IN MARGINAL LANDS) Block Plantation Railway Plantation Agroforestry Embankment Plantation Roadside Plantation Forest Types of Bangladesh Rubber plantation Bamboo groves Tea garden River Network of Bangladesh River Network of Bangladesh Bangladesh is a riverine country . About 800 rivers including tributaries flow through the country constituting a waterway of total length around 24,140 km Transboundary Rivers Total Rivers 57 With India 54 With Myanmar 3 Wetlands of Bangladesh Total area of wetlands throughout Bangladesh exceeds 8 million ha. i.e., about 50% of the total national land. Less than 10% of the total water flow originates from country’s own catchments and rest comes from India, Nepal and Bhutan. River Karnaphuli is the principal river of CHT & Chittagong oiginating from the Lushai hills in Mizoram State of India, flows 270 km southwest through Rangamati to empty into the Bay of Bengal, through Port City Chittagong. The dam has a 745 feet (227 m) long spillway containing 16 gates. Through the spillway 5,250,000 cu ft/s (149,000 m3/s) of water can pass. The Kaptai Lake The Karnaphuli River, was dammed in 1962 primarily for development of hydroelectric power, flooding an area of about 68,000 ha, to become the Kaptai Lake. It is the largest man-made freshwater lake in Bangladesh. The dam has a 745 feet (227 m) long spillway containing 16 gates. Through the spillway 5,250,000 cu ft/s (149,000 m3/s) of water can pass. The Kaptai Lake The lower part of the Kassalong River, major tributary of the river Karnaphuli, has formed the lake. The lake is “H” shaped, bearing two arms, joined by a narrow gorge. The Karnaphuli, Kassalong & Myani Rivers feed the right arm and The Chengri and the Rainkhiong Rivers feed the left arm. The dam has a 745 feet (227 m) long spillway containing 16 gates. Through the spillway 5,250,000 cu ft/s (149,000 m3/s) of water can pass. The Kaptai Lake Watershed Kassalong RF 137863 ha Maini Headwater RF 21586 ha Rainkhiong RF 76330 ha Sitapahar-Rampahar RF 5876 ha Borkol RF 203 ha TOTAL FOREST WATERSHED 2,71,658 ha Unclassified State Forests (USF) & Other land use is roughly double of the Forested Watershed area Topography, Soil & Climate Most parts of this watershed are mountainous with some up to 2438 m MSL. The beautiful landscape is comprised of semi-consolidated and consolidated rocks, possessing steep slope of elevation ranging from 350 to 1 000 m above MSL. The soils are mainly acrisols in the hills and lixisols in the valleys. Climate No. Months Average of rainfall rainy days Min. air Relative Max. air temperature temperature humidity (%) (°C) (°C) Evaporation (mm) Wind velocity (km/hr) Seasons considered for this study Jan 7.2 2 26.4 15.7 70 104 3.2 Feb Mar Apr 19.4 29.8 33.4 2 3 4 29.1 31.5 32.7 18.5 22.4 25.2 66 63 61 76 83 79 3.5 5.8 9.1 May 238.6 10 32.9 26.1 69 76 9.3 Jun 165 13 32.1 26.3 83 85 8.2 Jul Aug 295.5 275.3 15 15 32.4 32.6 26.4 26.3 85 82 82 130 7.9 Wet season 7.3 Sep 143 13 31.6 25.9 88 119 5.7 Oct 87.6 8 32.6 22.8 86 107 3.7 Nov 27.3 3 30.6 25.2 72 78 1.9 Dec 1 1 27.4 17.1 73 106 1.8 Source: Dry season Dry season Multipurpose Kaptai Lake Requirement of water level: 27.07 m MSL is required for safe operation of the power plant . below 24.38 m MSL the generation of hydro electricity power disrupted. When the water level falls below 22.25 m MSL the generation of hydro-electricity is ceased at all five units of the 230-MW plant. Water level status & requirement 35 33.22 m MSL 30 27.07 24.38 25 20.11 22.25 20 15 10 5 0 Max. Min. Safe Disrrupt Cease Water level Multipurpose Kaptai Lake It also plays a vital role for Navigation Agriculture Sports Fishery Recreation Control deadly floods due to torrential monsoon rain Shifting cultivation: Threats to Kaptai Lake Shifting cultivation reduced the natural system of soil conservation. • 60,000 families use 85,000 ha of the hill forests • Soil loss 26–68 t ha-1 yr-1 Deforestation: Threats to Kaptai Lake Except the Kassalong RF and Rankhiang RF, the almost entire watershed area of the lake has been deforested. As a result, the hill lands are mostly covered with scrubs which include scattered trees of different species, bamboos, grasses and shrubs. For this reason, soil cover has been exposed and rainwater easily causes soil erosion, severe run-off and landslides during monsoon. Human settlement: Threats to Kaptai Lake Growing agriculture: Threats to Kaptai Lake Population pressure increased in the vicinity of the Kaptai Lake for swallowing most of the best valley-bottom land for cultivation. Unscientific cultivation causes soil erosion. Massive teak plantation: Threats to Kaptai Lake Besides, there are concerns that teak plantations cause excessive erosion and soil depletion. RESTORATION & REHIBILITATION FD initiated in 1980s a rehabilitation programme for Jhumias RESTORATION & REHIBILITATION Between 1990 and 2010 about 33000 ha of forest plantations were raised. RESTORATION & REHIBILITATION 2300 shifting cultivator families have been settled. Another 6,500 households were rehabilitated by the Chittagong Hill Tracts Development Board. Each family allotted 2 ha land for housing & horticulture, also cash capital for Alternate Income Generation. RESTORATION & REHIBILITATION The projects have provided alternatives to jhum cultivation, particularly home gardening since the 1980s. MATERIAL AND METHODS Sampling sites FOUR sampling stations were selected : Station s Description A A point of the lake beyond main stream, surrounded by forested areas (Barkal) B A point of the lake beyond main stream, surrounded by degraded areas (Barkal) C A point of the main channel passing through forested areas (Nannerchar) D A point of the main stream passing through degraded areas (Nannerchar) MATERIAL AND METHODS Sampling Water samples were collected from 0.2D and 0.8D of the crosssection at three equal distance points using water samplers (DoF, Bangladesh). MATERIAL AND METHODS Physicochemical analysis of water samples Water samples were analyzed to obtain readings on following physicochemical properties of lake water : 1. pH (TOA pH Meter) 2. TSS (filtering, drying & weighing method) 3. Turbidity (Geopack Digital Turbidity Meter) 4. DO (measured by Jenway 970 DO2 Meter) 5. BOD5 (difference between initial DO and 5 day DO measured by DO2 Meter), and 6. Velocity (was measured by Geopack Digital Velocity Meter) Results pH 7 6 pH Value 5 4 A 3 2 1 0 Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Sampling stations pH ranged from 5.3-6.2 and 5.1-6.1 in station A and station B, respectively with low pH value in station B during wet season. Although these small changes in pH are not likely to have any direct impact on aquatic life, they greatly influence the availability and solubility of all chemical forms in the lake and may aggravate nutrient problems. Total Suspended Solids (TSS) 2000 1800 1600 TSS (mg/L) 1400 1200 1000 A 800 B 600 400 200 0 Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Sampling stations TSS ranged from 121.1 to 1358.4 mg/L and 126.3 to 1793.2 mg/L in station A and station B, respectively with higher quantity of TSS in station B during wet season. Turbidity 900 800 700 NTU 600 500 400 A 300 B 200 100 0 Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Sampling stations Turbidity ranged from 123.1 to 745.3 NTU and 145.5 to 825.8 NTU in station A and station B, respectively with higher turbidity in station B during wet season. Dissolved oxygen (DO) 8 7 DO (mg/L) 6 5 4 A 3 B 2 1 0 Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Sampling stations DO varied between 6.0 mg/L to 7.3 mg/L and 5.1 mg/L to 6.9 mg/L in station A and station B, respectively with lower DO in station B throughout the year except during rainy period. Biological Oxygen Demand (BOD5) 12 A B BOD5 (mg/L) 10 8 6 4 2 0 Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Sampling stations It varied between 5.1 mg/L to 8.3 mg/L and 5.7 mg/L to 10.2 mg/L in station A and station B, respectively with higher BOD in station B throughout the year. During wet season BOD was comparatively higher in both the stations. Velocity of stream flow 3.5 3 Similar variation in velocity was observed in the cross-section of main channel C (1.16 to 2.89 m/s) and D (1.08 to 3.32 m/s). 2.5 Velocity (m/s) Velocity of stream flow is slightly low (0.04 m/s) at B cross-section during dry season as compared to that from A cross-section. (0.05 m/s) Conversely, it is high during wet season at B cross-section (0.63 m/s). 2 A B 1.5 C D 1 0.5 0 JAN FEB MAR APR MAY JUN JUL AUG SEP OCT NOV DEC Sampling stations DISCUSSIONS Excessive TSS and higher turbidity where the lake-bank was devoid of vegetation and under shifting cultivation indicates high rate of siltation to shorten the life-time of the lake. The situation is further aggravated during the monsoon. On the other hand the lake passing through its watershed with forest plantations and controlled shifting cultivation exhibited comparatively better physicochemical properties The results indicates that tree cover retards run-off and soil erosion and help maintain water quality and influence stream flow. Further in-depth study will generate data to help impress policymaker to bring the watersheds of Kaptai Lake under forest plantation programmes, control of shifting cultivation and adoption of policy for environmentally sustainabale agriculture. CONCLUSIONS Massive tree restoration programmes in the vital watersheds, and forestry practices should be planned in such a way that the forest production, and water yield and quality are in complete harmony. ACKNOWLEDGEMENTS Forestry Development & Training Centre, Kaptai Pulpwood Forest Division, Kaptai Karnaphuli Hydro Power Station Authority, Kaptai Bangladesh Water Development Board Bangladesh Department of Fishery THANK YOU