基于空间图像的穆罕平原盐渍化地区勘探

Meherremlı Latafat
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引用次数: 0

摘要

目的:研究的主要目的是exploratıon的salıned地区ın的mughan plaın上basıs的空间pıctures。方法:本文以漠干平原盐碱区为研究对象。该研究是为了将卫星图像分析结果与该地区的实际情况进行比较。研究的结果是,编制和评价了该地区的各种地图。结果:平原形成的历史为解释该地区土壤中盐的积累提供了一个必要的机会。里海西部海湾在第四时期以前就存在了,这是它的侵略和退步的结果,无疑是领土盐碱化的一个主要因素。地质物质分析表明,覆盖共和国平原的山系含盐沉积物受外部和内部因素侵蚀,在地表和地下水流的影响下被带到该地区倾斜程度较低的地区。地表水主要指从山坡流出的水。在这种情况下,进口盐的数量和化学成分当然首先取决于被侵蚀岩石的盐度及其化学成分,而这又与该地区的地质历史密切相关。在低坡度地区,流向这部分斜坡的洪泛水流在沿着地表移动时,溶解了所经过地区的盐,从而增加了溶液的密度。另一方面,从斜坡上部流向内陆的溪流密度也在这里增加。在这两种情况下,雨洪流都在场地倾斜程度较低的部分流向地面,从而降低了它们的流速。最后,浸泡在土壤中的溶液在高温气候下再次蒸发,造成不同程度的盐度,这取决于它所含盐分的数量。科学新颖性:获得的科学结果将有助于保护里海平原景观的生态多样性,并优化景观的自然资源潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
EXPLORATION OF SALINED AREAS IN THE MUGHAN PLAIN ON THE BASIS OF SPACE PICTURES
Aim: the main aim of the study is exploratıon of salıned areas ın the mughan plaın on the basıs of space pıctures. Methodology: The article is based on a study of saline areas in the Mugan plain. The study was conducted to compare the results of satellite imagery analysis with the actual situation in the area. As a result of the research, various cartographic maps of the area were compiled and evaluated. Results: The history of the formation of the plain provides a necessary opportunity to explain the accumulation of salts in one way or another in the soils of the area. The western gulf of the Caspian Sea, which existed before the fourth period, as a result of its transgression and regression, was undoubtedly a major factor in the salinization of the territory. Analysis of geological materials shows that the saline sediments in the mountain systems covering the plains of the republic are eroded by external and internal factors and brought to the less inclined areas of the area under the influence of surface and underground currents. Surface water refers mainly to water flowing from mountain slopes. In this case, both the amount and chemical composition of the imported salts, of course, depends, above all, on the salinity of the eroded rocks and their chemical composition, which in turn is closely linked to the geological history of the area. In low-slope areas, deluvial currents flowing to this part of the slopes increase the density of the solution by dissolving the salts found in the areas they pass through as they move along the surface. On the other hand, the density of streams moving inland from the upper parts of the slopes also increases here. In both cases, the deluvial currents flow to the ground in the less inclined part of the field, reducing their flow velocity. Finally, the solution soaked in the soil evaporates again in high-temperature climates, causing varying degrees of salinity, depending on the amount of salts it contains Scientific novelty: The obtained scientific results will enable the protection of the ecological diversity of landscapes on the plain of the Caspian Sea and optimize natural resource potential of landscapes.
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