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Characteristics and Causes of Gully Erosion in Iran

机译:伊朗沟壑侵蚀的特征及成因

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摘要

A research plan is going to start to study the characteristics and causes of gully initiation. To set up its methodology, a questionnaire was designed and tested by experts in the field in 1998 and 1999 in five provinces with different physical and socio-economic conditions. The pre-results indicate that gullies are initiated in different ecological and climatological conditions. Their view plans are dendretic with U-shaped cross section and medium size with respect to their depth. The vertical profile of the headcuts is dominantly vertical, that is the activity of surface runoff is important. The results reveal that the important factors in gully initiation are deterioration of vegetation cover, flood and rainfall intensity and mismanagement of watersheds. Important on site damages are disconnection of rural roads and bridge breakage, land scoring, recession of water table, immigration of rural people and movement of the location of villages. At this stage it seems that the combination of high intensity rainfall with ground surface disturbance by road construction and deterioration of native vegetation cover are the most important factors for gully initiation. Surface runoff would be the dominant hydrological process in gully development.
机译:一项研究计划将开始研究沟壑引发的特征和原因。为了建立其方法,该调查表由该领域的专家在1998年和1999年在五个具有不同自然和社会经济状况的省份中设计和测试。结果表明,沟壑是在不同的生态和气候条件下引发的。他们的视图平面呈U型横截面,相对于深度而言大小适中。截割的垂直轮廓主要是垂直的,也就是说,地表径流的活动很重要。结果表明,沟壑形成的重要因素是植被覆盖度下降,洪水和降雨强度以及流域管理不善。重要的现场损害是农村道路的断开和桥梁的破损,土地的划伤,地下水位的下降,农村人口的移民以及村庄所在地的移动。在这一阶段,高强度降雨与道路建设对地面的干扰以及原生植被的退化相结合,似乎是沟壑萌发的最重要因素。地表径流将是沟壑发育的主要水文过程。

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