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Detection and Assessment of the Waterlogging in the Dryland Drainage Basins Using Remote Sensing and GIS Techniques

机译:利用遥感和GIS技术对干旱地区流域内涝的检测与评估

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Waterlogging and elevated soil salinity commonly develop in the cultivated and arable areas of the Sahara, particularly within closed drainage basins. Multi-temporal remote sensing data of the Landsat Thematic Mapper (TM) and Enhanced Thematic Mapper (ETM+) for the Farafra Oasis in the Western Desert of Egypt were collected and processed to detect land cover changes, cultivations, and the extent of water ponding and seepage channels. The Shuttle Radar Topography Mission (SRTM) Digital Elevation Model (DEM) has been processed to delineate catchment morphometric parameters and to examine the spatial distribution of cultivated fields and their relation to the extracted drainage networks. The soil of these closed drainage basins is mainly shallow and lithic with high calcium carbonate content. Therefore the downward percolation of excess irrigation water is limited by the development of subsurface hardpan, which also saturates the upper layer of soil with water. The subsurface seepage from the newly cultivated areas in the Farafra Oasis has revealed the pattern of buried alluvial channels, which are waterlogged and outlined by the growth of diagnostic saline shrubs. Furthermore, the courses of these waterlogged channels are coinciding with their counterparts of the SRTM DEM, and the recent satellite images show that the surface playas in the downstream of these channels are partially occupied by water ponds. The geomorphology of closed drainage basins has to be considered when planning for new cultivation in dry land catchments to better control waterlogging hazard. Accordingly, several management strategies can be adopted to combat land degradation by water logging including; cultivation of certain areas and localities within each drainage basins, and conveying the drainage and seepage water through the inactive alluvial channels into abandoned playas, which are reserved for evaporation. Moreover, farm management and balancing irrigation water, salt leaching, and evap- -transpiration are also critical to lessen the development of waterlogging.
机译:撒哈拉沙漠的耕地和耕种地区,特别是在封闭的流域内,通常会发生涝灾和土壤盐分升高。收集并处理了埃及西部沙漠中Farafra绿洲的Landsat专题测绘仪(TM)和增强型专题测绘仪(ETM +)的多时相遥感数据,以检测土地覆盖变化,耕种以及蓄水和蓄水的程度。渗水渠道。已对航天飞机雷达地形任务(SRTM)数字高程模型(DEM)进行了描述,以描绘集水区形态参数并检查耕地的空间分布及其与提取的排水网络的关系。这些封闭的流域的土壤主要是浅层和石质的,碳酸钙含量很高。因此,过量灌溉水的向下渗透受到地下硬盘的发展的限制,硬顶也使水的上层饱和。 Farafra绿洲新近种植区的地下渗漏揭示了地下冲积河道的格局,这些河道被淹没,并被诊断性盐灌木的生长勾勒出轮廓。此外,这些淹水河道的路线与SRTM DEM的对应路线一致,最近的卫星图像显示,这些河道下游的地表径流部分被水塘占据。在规划旱地集水区的新种植时,必须考虑封闭流域的地貌,以更好地控制涝灾。因此,可以采取几种管理策略来应对因涝灾造成的土地退化。在每个流域内种植某些区域和地方,并将排水和渗水通过非活跃的冲积渠道输送到废弃的普拉亚,这些普拉亚保留用于蒸发。此外,农场管理和平衡灌溉水,盐分浸出和蒸腾作用对于减轻涝灾的发展也至关重要。

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