Evaluating two possible solutions to immobilize drift sands in the Sub-Aral region 1 Contents 1. Introduction..................................................................................3 2. Problems......................................................................................4 Environmental damage .......................................................4 Health effects.......................................................................4 3. Possible solutions.........................................................................6 Carboxymethyl cellulose, straws and the salt-resistant plants………………………...........................................................6 Planting the saxaul...............................................................7 4. Evaluation of possible solutions ………………………….........................8 5. Conclusion....................................................................................9 6. List of References........................................................................10 2 Introduction Once the Aral Sea was the world’s fourth-largest lake; it was famous for its rich natural resources, and Sub-Aral flora and fauna used to be prosperous and rich. Since the 1960s, the Aral Sea has been drying out, because its two main rivers Amu Darya and Syr Darya have been overused for irrigation. This has led to serious problems as large amounts of river water could not reach the sea due to irrigation or were lost in sands. 1962 was the start for a catastrophic drying out of the sea. Since 1962 the Aral Sea’s area reached 36 thousands kilometres squared, that is three times smaller than at the beginning of the 1960s. Moreover, the sea level has dropped to 14m compared to that period of time. Salinity has increased significantly as water level has decreased to 70%, leaving approximately 2.7 million hectares of open shores (Wiggs et al, 2003, p.142). The desiccated sea bottom has already got its name – Aralkum desert whose surface consists of salt and mineral remnants, washed from irrigated fields. This situation is becoming dangerous due to the location of the sea. The Aral Sea undergoes of strong winds that predominantly blow from west to east, and spread vast amounts of salt thousands kilometres away from the sea (Wiggs et al, 2003, p.142). 3 Figure 1. Aral Sea water level from 1989 to 2003 (TERRA satellite, NASA). Figure 1 illustrates dramatic changes in the Aral Sea’s water levels between 1989 and 2003 taken by MODIS spectrometer from the TERRA satellite. During this period the water level in the Aral Sea has decreased by 5 times according to NASA estimations. It is known that drift sands of the Sub-Aral area and Aral’s drained bottom are over salted. The most worrying factor, which is causing environmental damage, is drifting of salts and dust with wind from the Sub-Aral area, which is approximately 75-100 million tonnes every year (Meshkov et al, p.118). Consequently, it is important to find ways to fix salty sands and create hard soil crusts, which will prevent corrosion from spreading and allow plants to live in the Sub-Aral area. Water resistant macrostructure of the salty sands is over 0.25mm, which is considered very small number (Ali, 2011, p.30). These 4 macrostructures have a significant influence on the salt resistant plants cultivation. Hence, planting salt-resistant plants and saxaul could prevent wind erosion and fix drift sands. The aim of this essay is to examine two ways of preventing drift sands in the Sub-Aral region from wind erosion. First, the use of chemical fastening substances such as water-soluble polymer Carboxymethyl cellulose (CMC) and straws, and planting the salt-resistant plants Agropyron cristatum will be discussed. The second solution to the Aral problem could be planting the saxaul. Environmental damage Suspended solids in the form of aerosols with agricultural pesticides, fertilizers and other harmful components of industrial and municipal wastes prevail in the composition of the winds. One of the dangerous consequences of the drying out of the Aral Sea is the increasing degradation of mountainous glaciers. Intensive melting of glaciers occurs because of the increase of dust on glacier surfaces and mineralization of precipitation on them (Glants & Zonn, 2005, p.17). Regional climatic changes have also resulted directly from atmospheric and ecological changes in the Aral Sea’s basin. These changes include a reduction in rainfall and changes in regional wind flow patterns aloft and at ground level. The reduced size of the sea surface means that the Aral Sea was not able to moderate the harsh effects of the cold winds from Siberia or to reduce heat extremes in the summer time. Furthermore, the growing season was 5 shortened, pasture productivity cut in half and precipitation along the seashore was reduced considerably (UNEP/GRID, 1998). Health effects Since the drying out took place the population health changed for the worse in the Aral Sea Basin. The negative effects occurred because of the Aral Sea environmental problems including water contamination, air pollution, lack of portable water and low sanitation levels. Left behind population of the Sub-Aral region struggled to maintain living conditions in a landscape that suddenly turned hostile. This is an issue of the day in the Aral Sea Basin and neighbouring regions. Throat cancer and respiratory diseases became common, and with no reliable protein source in the absence of fish, thousands became anaemic. Maternal and infant mortality rates in the epicentre of the Sub-Aral zone are one of the highest in CIS countries. Decrease of life expectancy, high rate of tuberculosis, anaemia, cancer, asthma, dysfunction of thyroid gland, blood-, heart-, kidney- and liver-diseases cases were observed (Small et al, 2001, p.547). This led to worsening of genofund. The situation is aggravated by inadequate prevention measures, morbidity monitoring and inaccessibility of necessary medicines in the Aral Sea region. 6 Table 1. Concentrations of metals in children hair from the Aral Sea region (mg/kg) Aral Sea region Hamburg region Lead 15 0.5 Manganese 12.3 2.0 Aluminium 20.8 12 From the Table 1 it can be noted that "the lead level in the hair of the Kazakhstani children was 30 times higher than the upper limit in hair from children in Hamburg in West Germany" (Jensen et al, 1997, p.192). Table 2. Concentrations of lead and cadmium in children blood from the Aral Sea region (µg/l) Sample Aral Sea Lead Cadmium 1 187 0.50 2 160 0.57 3 150 0.70 Table 2 shows that "In the erythrocytes the lead concentration was approximately 5 times higher than in children from Stockholm in Sweden". Swedish standards: lead - 30 medium (range 13-79); cadmium - 0.24 medium (range 0.18-0.30) (Jensen et al, 1997, p.192). The Aral Sea area is confronted with a crippling water crisis. The lack of 7 availability of water is a particular reason for the death of the Aral Sea and for the associated litany of negative ecologic and human health effects. Many fish species in the sea, which were an important economic and nutritional element in the region, have become extinct them (Glants & Zonn, 2005, p.17). Not surprisingly, the quality of water for human consumption is poor. Those processes that have contributed to the sea desiccation - over-irrigation and water mismanagement - also resulted in a rise of the groundwater table, which then have become contaminated with high levels of salts and other minerals. Groundwater quality ranges from a minimum of 0.4 g/l total dissolved salts (TDS) to an astounding 4-6 g/l. According to World Health Organization (WHO), worldwide standard for water mineral content acceptable for human consumption is 1.5 g/l TDS (Ataniyazova, 2003, p.2). Possible solutions: Salt-resistant plants Problems of the Aral Sea could be solved by using chemical fixing substances. The efficiency of the chemical method depends mostly on a fixing substance which enables particles to interconnect and work together. Carboxymethyl cellulose (CMC) can be used as a fixing substance, or it can be mixed with agricultural wastes (straws). Table 3 shows that the best mix of CMC and compost is 2% and 4% of CMC combined with 7 tonnes of straws (Ali, 2011, p.32). 8 Table 3. Increase percentages for organic matter contents of treated soil (Ali, 2011, p.29). 2% of CMC with 5 ton of compost 48.78 % 4% of CMC with 5 ton of compost 63.41 % 2% of CMC with 7 ton of compost 100 % 4% of CMC with 7 ton of compost 102 % It should also be mentioned that CMC has other positive features such as inexpensive price (ibid, p.24) and easy access. This is due to large-capacity manufactures of CMC, which are mostly wastes of cotton gin plants, based in the Republic of Kazakhstan. CMC forms viscous solutions at low concentration. Moreover, it is a bio-decomposed polymer and is made out of natural polymer – cotton cellulose (ibid, p.24). There is also a proven example of fixing drift sands with the use of wheat straw for the chemical composition. It is a renewable waste, produced annually. Generally, millions tons of it are either earthed or burnt, thus causing environmental damage. Figure 2. Agropyron cristatum (Retrieved from http://www.forestryimages.org/browse/detail.cfm?imgnum=1459834 ) 9 Agropyron cristatum (shown in Figure 2) is a crested wheat grass that represents a species in the Grass family (Poaceae). This plant is often used for forage and erosion control. Agropyron cristatum is a highly competitive and persistent plant in drier areas, and has a moderate ability to spread by seed (USDA, 2006, p.1). Using salt-resistant plants such as Agropyron cristatum will facilitate the development of livestock; consequently, it could improve the wealth of local people and create soil conditions for natural colonization. According to Ali (ibid) free disperse sand system changes into viscously disperse aggregated system because of the influence CMC complex mixture and wheat straws. They have a positive influence on hydro-physical properties of the soil such as diminishing soil bulk concentration and preventing macro porosity. Thus, pores, that hold water, are growing, whereas the mean diameter of soil pores is lessening causing soil to preserve more moisture. This is also called hydraulic conductivity. Moreover, the cure applied on soil chemical assets resulted in minor shrink of soil pH and raise of organic content. An increase in soil nutrient substances such as nitrogen, phosphorus and potassium was also noted (Ali, 2011, p.23). Planting the saxaul The ecosystem of saxaul pastures, that were the richest in biological productivity of the Aral Sea, have undergone human negative impact in recent years. In 90’s felling saxaul for heating needs by the local population became an 10 issue as created a threat of a complete destruction of the Haloxylon aphyllum (saxaul) and Haloxylon persicum ecosystems. As a result, 60% of the saxaul region is experiencing a severe degradation process (Orlovsky, Birnbaum, 2002, p.234). Excessive felling of trees and shrubs in the area of runoff formation resulted in the increase of negative processes such as floods, mudflows, landslides, lack of water. Figure 3. Saxaul (Retrieved from http://www.plantarium.ru/page/image/id/40287.html) Saxaul tree (shown in Figure 3) is spongy and absorbs moisture through the bark, so the water can be extracted, which is a critically important commodity for people of the deserts. Saxaul also supplies cover and forage for wildlife, for instance, camels, sheep and various bird species (ibid, p.235, 239). Saxaul is used in medicine as an antidote and also as a cure for gastrointestinal-tract diseases (Baisalova, Erkasov, 2011, p.1). Saxaul forest regions which are located near urban areas, is predicted to be a source of income for farmers and a source of additional supplies of wood. However, there is a great risk that planted saxaul will be used by the local population as a fuel source due to the 11 fact that the city has not developed a gas network yet. The activities of afforestation, planting, care and development of forest resources could increase the employment of local population, which is one of the main benefits. Hence, this might also result in the income increase of local people. The new shrubs, bushes, and plants capture rain and snow that are crucial in the drought-affected Aral region whose current annual precipitation averages only 150-200 millimeters (UNEP/GRID, 1998). Saxaul has a deep and well-developed root system. The roots of the plant grow parallel to the ground and fasten to the mixture of sand, dust and salt. Thus, saxaul prevents further erosion and is capable of absorbing water from soils with very low moisture content, while the upper part of the plant acts as a windbreaker, decreasing wind velocity (Orlovsky, Birnbaum, 2002, p.235). Evaluation of possible solutions There is no lack of saxaul seeds in Kazakhstan and the zone of saxaul forests occupies almost 50% of the Republic’s territory and has an area of 10.17 million hectares (Orlovsky, Birnbaum, 2002, p.234). One of the advantages of saxaul is that once it is planted, it will be there for years. Moreover, it is a reasonably fast growing species and particularly rapid growth is noted in its root system, which, in 3 years, reaches up to 5 meters deep and can penetrate 10 meters into the ground. CMC polymer is bio-decomposed polymer, and since the Republic of Kazakhstan has obtained large-capacity manufactures of CMC, 12 it is inexpensive and easily accessible (Ali, 2011, p.24). However, the CMC factories are located 300 kilometres away from the Aral Sea. Therefore, transport costs are needed in order to send the polymer to the Sub-Aral region, which could significantly add to the cost of the product. Thus, using seeds and planting saxaul could be much cheaper than using CMC. Using the CMC polymer with wheat straws and salt-resistant plant as well as planting saxaul appear to be the best possible solutions to immobilize drift sands in the Sub-Aral region. These methods create hard soil crusts that will not prevent plants from growing, but prevent corrosion from spreading. Consequently, the number of dust storms will decrease, so population health will change for the better as air pollution is predicted to reduce. Biological productivity of arid areas will increase and finally the climate change could become sustainable and heat extremes in the summer time may be reduced. From the research it can be seen that both solutions have only positive effects on the environment (Orlovsky, Birnbaum, 2002, p.235). The activities of afforestation, planting, care and development of forest resources will increase the employment of local population, which is one of the main benefits. Moreover, the plants may also provide an alternative fodder source for animal production, thereby increasing agricultural productivity. In other words, both solutions will increase employment as well as the wealth of local residents. In this essay two possible solutions were compared in terms of the 13 following aspects: cost, environmental effects and employment. From the environmental side, both solutions show only positive effects. They are ecologically-friendly and the common feature of Agropyron cristatum and saxaul plants is their high adaptability to adverse climatic conditions such as hot dry summers, cold winters, low humidity and shifting sands. Furthermore, implantation of these plants will require labour force. Hence, employment of people in the Sub-Aral region will increase their prosperity and possibly the standard of living will rise. However, expenses related to the application of these methods differ. As for saxaul the only thing that is needed is seeds, whereas for CMC and wheat straws transportation to the Aral Sea is required. Therefore, from the research it can be seen that it is cheaper to use saxaul than CMC water-soluble polymer and wheat straws. Conclusion Two methods of preventing the eolation process of sand dust aerosol drifting were examined. The first method is based on using chemical fastening substances, consisting of a CMC water-soluble polymer and wheat straws as well as the planting of the salt-resistant plant agropyron cristatum. The second technique studied is the planting of saxaul. The former method is a chemical way to fix drift sands of the Aral Sea with the help of complex additives, consisting of a CMC with agricultural wastes – wheat straws, preventing corrosion and helping to improve ecological conditions in planted areas of the 14 Sub-Aral and in the Aral Sea’s drained bottoms. This has two positive features such as solving ecological problems and waste utilization. Similarly, planting the saxaul in the Sub-Aral region will contribute to solving important social and environmental issues. This will result in the reconstruction of the past forage base for livestock and fixing large areas of the dried bottom. The elimination of the hearts of salt and dust removal will improve the environmental situation at the local and regional levels. Appearance of a stable vegetation cover will create a kindly micro-climate and soil conditions for natural colonization. All in all, immobilizing drift sands in the Sub-Aral area by planting saxaul is considered to be the most suitable and the cheapest way. 15 List of References: Ali, L. (2011). Significance of Applied Cellulose Polymer and Organic Manure for Ameliorating Hydro-physico-chemical Properties of Sandy Soil and Maize Yield. Australian Journal of Basic and Applied Sciences, 5(6), 23-35. 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