Analysis physical and chemical properties of soil and morphometric impacts on gully erosion

Desert Pub Date : 2017-12-20 DOI:10.22059/JDESERT.2017.64179
S. A. Saraskanroud, B. Zeinali, V. Mohammadnejad
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引用次数: 6

Abstract

It is widely known that the development of gullies causes the loss of a great amount of soil and can be considered as one of the principal causes of geo-environmental degradation. The study area of the present research is located in the eastern shores of Urmia Lake. This study sought to evaluate the rate of growth and effective factors on the area’s gully dynamic over a year. To achieve this goal, levels of Electrical Conductivity (EC), Sodium Adsorption Ratio (SAR), pH, types of soil, and morphometric analysis were used for categorizing and analyzing effective factors on the creation of gully erosion. In addition, as the climate index, the coefficient of moisture in the area’s formation for analyzing the area’s gully erosion potential was also employed as relevant indicators. The results based on climate indices show that the area’s gully erosion potential is high. Analyzing the taken samples’ structures indicated that the constructing components of geological formations provided highly appropriate conditions for vertical and horizontal leveling of gullies because of the weak building of aggregates in a way that the results of the morphometric monitoring of the gullies represent the area’s high growth speed and dynamicity. High accumulation of soluble salts especially high values of SAR and EC have led to dissolution erosion that provides the conditions for creating tunnel erosion. The results of the research showed gully erosion formation in the study area and its expansion due to two factors, climate factors together with the chemical and physical characteristics of ‌an area’s soils. The results of the present research are of great importance for gully erosion modeling tasks in the study area and can be used as the base of future researches for identifying the relevant criteria and indicators in gully erosions.
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土壤理化性质分析及形态计量学对冲沟侵蚀的影响
众所周知,沟渠的发展造成了大量土壤的流失,是导致地质环境退化的主要原因之一。本研究的研究区域位于乌尔米亚湖东岸。本研究旨在评估一年内该地区沟谷动态的增长率和有效因素。为了实现这一目标,利用电导率(EC)、钠吸附比(SAR)、pH值、土壤类型和形态计量学分析对沟蚀形成的有效因素进行分类和分析。此外,作为气候指标,还采用该地区地层水分系数作为分析该地区沟槽侵蚀潜力的相关指标。基于气候指数的研究结果表明,该地区沟沟侵蚀潜力较大。通过对所采样品结构的分析,发现地质构造的构造成分为沟槽的垂直和水平平整提供了非常适宜的条件,因为聚集体的构造较弱,沟槽的形态监测结果反映了该地区的高生长速度和动态性。可溶性盐的大量积累,特别是SAR和EC的高值导致了溶蚀,为隧道侵蚀的形成提供了条件。研究结果表明,研究区沟蚀的形成和扩大主要受气候因素和土壤理化特性的影响。研究结果对研究区沟壑侵蚀建模具有重要意义,可作为今后研究确定沟壑侵蚀相关准则和指标的基础。
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