首页> 外文期刊>Journal of Water Resources and Ocean Science >Overview to Potential Sources, Soil Salinization and Expansion Level of Lake Basaka, Central Rift Valley Region of Ethiopia
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Overview to Potential Sources, Soil Salinization and Expansion Level of Lake Basaka, Central Rift Valley Region of Ethiopia

机译:埃塞俄比亚中央裂谷地区湖巴湖潜在来源,土壤盐渍化和扩建水平

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The aim of this overview is extended to indicate the Potential Sources, Soil salinization and expansion level of lake Basaka. Lake Basaka is located in the middle Awash River Basin, Central Rift Valley of Ethiopia at about 200 km south East of the capital city, Addis Ababa. The lake is expanding as opposed to the other rift valley lakes in Ethiopia, which are shrinking, Lake Basaka is found to be expanding at an alarming rate. This overview indicates the expansion area/level/ of the lake is challenging the socio-economics and environment of the region significantly. With this point of view the lake's expansion is due to the agricultural sugarcane farm land use type near Beseka Lake and mostly due to the increased ground water flux to the lake. The potential sources or ground water flux to the lake could be an increase of ground water recharge following the establishment of irrigation schemes in the region, subsurface inflow from far away due to rift system influence, and Lake Neotectonism. The significant expansion of Lake Basaka during the past 35 years started after the introduction of Matahara sugar state. The expansion is affecting both the ground water dynamics and soil salinization of the nearby sugarcane Plantation and, if it continuous, the sustainability of the plantation itself is under great risk. The future expansion of the highly saline lake may be aggravated towards the east and Northeast direction due to the topography of the area. This has the potential to displace Matahara town and impact the sugar Plantation during the next two-three decades years. Assuming the past trends, the lake isexpected to join Awash River, thereby impacting all downstream irrigation developments in the Awash basin, and affecting the livelihood of the people depending on the water resources of this basin. Generally, the lake's has poor water quality and its expansion rate damaging effect to the region, and mitigation measures are very important for sustainable lake management.
机译:该概述的目的延长以表明巴萨卡湖的潜在来源,土壤盐渍化和扩建水平。萨卡拉湖位于埃塞俄比亚的中央裂谷河流河畔埃希河畔埃塞俄比亚,大约200公里,在首都亚的斯亚贝巴东南约200公里。湖正在扩展,而不是埃塞俄比亚的其他裂谷湖泊,湖泊巴萨湖被发现以惊人的速度扩张。此概述表明湖泊的扩展区域/级别/水平挑战了该地区的社会经济和环境。凭借这一观点,湖的扩张是由于贝塞卡湖附近的农业甘蔗农场使用类型,大部分是由于湖泊的地下水量增加。湖泊潜在来源或地下水通量可能是在该地区的灌溉计划中建立灌溉计划之后的地下水补给的增加,由于裂谷系统影响以及湖新型植物,地下流入。在介绍Matahara糖状态后,过去35年湖萨卡拉的大幅扩张。扩张正在影响附近的甘蔗种植园的地下水动力学和土壤盐渍化,如果它连续,种植园本身的可持续性都存在很大的风险。由于该地区的地形,盐水湖的未来扩张可能会朝向东部和东北方向而加剧。这有可能在未来两年三十三年内迁移Matahara镇并影响糖种植园。假设过去的趋势,湖仍然是加入避难所的河流,从而影响了令霸盆地的所有下游灌溉发展,并根据这条盆地的水资源影响人民的生计。一般来说,湖泊的水质差,其对该地区的膨胀率损害效应,缓解措施对可持续湖泊管理非常重要。

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