Impact of overgrazing and climate change on the lake ecosystem in arid region

Uranchimeg Tserendorj, Baigal-Amar Tuulaikhuu, Ayunshsuren Chananbaatar, Khishigjargal Moonkhor, Oyuntuya Sharavjamts, Ariunsuren Purevee, Tumenbayar Purev, Dambadarjaa Naranbat, Tuvshinbayar Danzan, Orgilbold Myangan
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Abstract

Mongolia's geographical location, extreme climate, fragile ecosystems, agricultural dependence on climate requires adaptation to global climate change and smart usage of natural resources. The water level of most lakes in Mongolia had been steadily increasing from mid-1960s to 1995 and declining from 1996. The purpose of this study is to determine current condition by each ecosystem compartment in and around the Lake Duruutsagaan and to define cause of the lake shrinking and deterioration of ecosystem. The Lake Duruutsagaan ecosystem study was carried out in the following natural elements: climate, hydrology, hydrobiology, forest, soil, pasture, plant species composition, and animals. The lake surface area was slightly decreased by 24.21% from 10.02 km2 in 2003 to 7.59 km2 in 2017. The lake water is highly mineralized, probably due to increases of evaporation of water. Also elevated concentrations of some chemical elements are detected in the lake water, including Phosphorus (22.6 mg L-1) and Arsenic (198 mg L-1). The high concentration of these two elements shown different kind of pollution existed in the lake. Probably, arsenic content in lake water is related to the geological composition of surrounding area, but elevated concentration of P can be attributed to the nutrient pollution due to soil erosion in surrounding area of lake. Species diversity in this lake is limited and only a few species of crustaceans that can tolerate under high salinity and polluted condition are present. All of soil samples have a low content of clay particles (between 2.6-8.5%). According to the soil samples data, pasture land in study area is moderately 80.95%, strongly 7.04% deteriorated due to direct and indirect effects of overgrazing. Especially, natural regeneration is not observed in the forest area. According to the study results, current condition of Lake Duruutsagaan and its surrounding area is indicating the need for some protection and restoration management.
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过度放牧与气候变化对干旱区湖泊生态系统的影响
蒙古国的地理位置、极端气候、脆弱的生态系统、农业对气候的依赖,要求蒙古国适应全球气候变化,并明智地利用自然资源。蒙古大多数湖泊的水位从1960年代中期到1995年一直在稳步上升,从1996年开始下降。本研究的目的是确定杜鲁特萨甘湖及其周围各生态系统的现状,并确定湖泊萎缩和生态系统恶化的原因。从气候、水文、水生生物、森林、土壤、牧场、植物物种组成和动物等自然要素对杜鲁茨萨甘湖生态系统进行了研究。湖泊面积由2003年的10.02 km2减少到2017年的7.59 km2,减少幅度为24.21%。湖水是高度矿化的,可能是由于水蒸发的增加。湖水中还检测到一些化学元素的浓度升高,包括磷(22.6 mg L-1)和砷(198 mg L-1)。这两种元素的高浓度表明该湖泊存在不同类型的污染。湖水中砷的含量可能与周边地区的地质组成有关,而磷的浓度升高可能与湖泊周边地区土壤侵蚀造成的养分污染有关。该湖的物种多样性有限,只有少数几种甲壳类动物能忍受高盐度和污染的环境。所有土样粘土颗粒含量均较低(在2.6 ~ 8.5%之间)。土壤样品数据显示,研究区草地因过度放牧直接和间接影响而退化的比例为中度80.95%,重度7.04%。特别是,在森林地区没有观察到自然更新。根据研究结果,杜鲁特萨甘湖及其周边地区的现状表明需要进行一定的保护和恢复管理。
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