对西部沙漠 Al - Mohammadi 盆地谷地土地退化情况的实地评估

Noora Abdulateef Turki Alani, Moshtaq Ahmed Gharbi, Mohammed Musa Hammadi
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摘要

这项经常性研究旨在为阿尔梅赫梅迪河谷盆地的土地退化提供大量科学细节。由于该盆地拥有不同的形态、地质特征、气候模式、各种土地资源(如土壤、植被和水资源),因此被视为不同的地点。该流域面积为 1971.49 平方公里,在对该流域进行实地考察后,发现了不同的土地退化范围。因此,通过地貌术语将盆地土地划分为六个土地单元。这些术语是通过 Land sat 8 卫星图像的光学解释得出的。这些单元包括高原、平原、洼地、谷地、冲积扇、冲积平原。此外,还利用 GLASOD 对物理、生物、化学和盐碱劣化进行了实地调查。因此,利用表格地图解释了其原因并测量了土地单元内的退化量。研究结果表明,浑浊盆地的空间差异导致了河谷盆地与其他土地的不同。此外,研究还得出了该地区人类活动与自然之间的空间关系。
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Field Evaluation of Land Deterioration in Al - Mohammadi Basin Valley at Western Desert
The recurrent study was in including lots scientific details on land deterioration for Almehmedi valley basin. This basin is represented as distinguish sites because it possesses different morphology, geological properties, climate pattern, various land resources such as soils, vegetation and water resources. Conceptualization of this study was entirely prepared then results were different to discover the range of land degradation using field evolution on this basin, which its area was 1971.49 km2. Therefore basin lands were divided into six land unites via geomorphological terms. These terms were done using optical explanation on Land sat 8 satellite image. These unites are high plateaus, flat plateaus,  unbath, valleys, alluvial fans, flood plain. Moreover field investigation was applied using GLASOD physical, biological, chemical and saline deterioration. Thus, their cause was explained and measured the deterioration amounts within land units using tables  maps. The research study could clouded basin field spatial differences resulted in differing the valley basin from other  lands. Furthermore, it resulted in spatial relations amongst human iturimm and natural in this area.
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