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Degradation of Cultivated Soils in a Semiarid Area of Greece

机译:希腊半干旱地区的耕地退化

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摘要

The soil loss, which results from the erosion processes, will be very serious, if conservation measures are not going to be undertaken very soon in central Greece. The main causes, which induce erosion in the study area, are (1) Irrigation water, (2) Torrential rainstorm, (3) Slope inclination (4) Land use and agricultural practices. The rain erosivity which was estimated using the Foumier index (FI) after analyzing the meteorological dada of the studied area is low (class 1), which means the rain induced erosion is generally low. In fact this is not exactly the real situation. Very often torrential rainstorms of usually short duration cause intense erosion (120-150 ton · ha~(-1) · y~(-1)) with heavy damages to agricultural fields and infrastructure and must be taken seriously into consideration. The estimated volume of erosion in relation to slope degree is from 21 to 310 ton · ha~(-1) · y~(-1) for inclinations 3.5% - 25%. The interpretation of aerial photography and satellite imagery] together with image analysis and GIS helped in recognizing and mapping areas with soils of higher erodibility and thus more susceptible to erosion.
机译:如果不很快在希腊中部采取保护措施,那么由侵蚀过程造成的土壤流失将非常严重。在研究区域内引起侵蚀的主要原因是(1)灌溉水,(2)暴雨,(3)坡度(4)土地利用和农业实践。在分析研究区域的气象数据之后,使用Foumier指数(FI)估算的降雨侵蚀力较低(1类),这意味着降雨引起的侵蚀通常较低。实际上,这并不完全是真实情况。通常,持续时间短的暴雨会造成强烈侵蚀(120-150吨·ha〜(-1)·y〜(-1)),对农田和基础设施造成严重破坏,必须予以认真考虑。相对于倾斜度,侵蚀量估计为21至310吨·ha〜(-1)·y〜(-1)(倾斜度为3.5%-25%)。 [航空摄影和卫星图像的解释]以及图像分析和GIS有助于识别和绘制具有较高侵蚀性且因此更容易受到侵蚀的土壤区域。

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