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Impact of Anthropogenic Factor on Karst Landscape (Zemo Imereti Structural Plateau Case Study), Georgia, Caucasus

机译:人为因子对喀斯特景观(Zemo Imereti结构高原案例),格鲁吉亚,高加索的影响

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The Zemo Imereti (Chiatura) Structural Plateau covers the easternmost part of the western Georgia limestone belt and is the only region of the platform karst in the entire Caucasus. Zemo Imereti Plateau’s complex structural studies revealed that the karst landscape has been completely transformed due to human strong economic activities, mainly related to the manganese unplanned, predatory extraction. The ore mining process completely destroyed the soil and vegetation cover thus creating “anthropo-badlands”. Due to manganese open-cast mining, the layers located over limestones are almost totally removed and heavy rains stipulate intense washout of substances from loose rocks. Intense washout of manganese extracted from mines and high contamination of river water streams take place directly in the river beds. Karst sinkholes and wells are common in the plateau, which are often used as waste fills-storages by the local population. Contaminated underground karst waters flowing into the above mentioned landforms are directly related to the karst springs used by the population and occasionally cause their turbidity and contamination, which is also confirmed by our indicator tests. As a laboratory study of the samples showed, mineralization of underground karst waters in the study area is 1.5 - 3 times higher than similar values in neighboring karst areas, which should be explained by the widespread of manganese open pits in the feeding basins of underground karst waters. According to the materials obtained from our surveys and calculations carried out, karst (chemical) denudation (surface 64.2 - 190.6 m~(3)/km~(2)/year, underground 1.5 - 117.0 m~(3)/km~(2)/year) has been increased in the study area than in other karst regions of Georgia, which is also related to technologic factors.
机译:Zemo Imereti(奇星)结构高原覆盖了格鲁吉亚西部石灰岩皮带的东部,是整个高加索平台喀斯特平台的唯一地区。 Zemo Imereti Plateau的复杂结构研究表明,由于人类强大的经济活动,喀斯特景观已完全转化,主要与锰无计划,掠夺性提取有关。矿石采矿过程完全摧毁了土壤和植被覆盖,从而创造了“炭疽湾荒地”。由于锰开放式挖掘,位于石灰岩上的层几乎完全被移除,大雨规定了松散岩石的浓度的损失。从矿山中提取的锰和河流水流的高污染直接在河床上直接进行了激烈的冲洗。喀斯特下沉孔和井在高原中很常见,常用于当地人口的废物填充物。流入上述地貌的受污染的地下喀斯特水域与人口使用的喀斯特弹簧直接相关,偶尔会导致它们的浊度和污染,这也通过我们的指标测试确认。作为对样品的实验室研究表明,研究区的地下喀斯特水域的矿化比邻近喀斯特地区的类似价值高1.5-3倍,这应该由地下喀斯特饲养盆地的锰开放坑的广泛解释水。根据我们的调查和计算中获得的材料,喀斯特(化学)剥落(表面64.2-190.6 m〜(3)/ km〜(2)/年,地下1.5 - 117.0 m〜(3)/ km〜( 2)/年)在研究区已经增加而不是格鲁吉亚的其他喀斯特地区,这也与技术因素有关。

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