首页> 外文OA文献 >USO DE TÉCNICAS DE GEOPROCESSAMENTO PARA MAPEAR O POTENCIAL NATURAL DE EROSÃO DA CHUVA NA BACIA HIDROGRÁFICA DO RESERVATÓRIO DE CACHOEIRA DOURADA – GO/MG
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USO DE TÉCNICAS DE GEOPROCESSAMENTO PARA MAPEAR O POTENCIAL NATURAL DE EROSÃO DA CHUVA NA BACIA HIDROGRÁFICA DO RESERVATÓRIO DE CACHOEIRA DOURADA – GO/MG

机译:利用地质处理技术绘制Cachoeira Dourada水库-GO / MG水文盆地的自然侵蚀潜力

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摘要

Natural potential erosion were defined from their main naturalconditioners in the region of hydrographic basin of CachoeiraDourada (between Goiás and Minas Gerais states −Brazil), withgeoprocessing techniques and the Universal Soil LossEquation (USLE). Upon the decision for natural erosionpotential, a matrix with values of erosivity (R), erodibility (K),declivity, and ramp length (LS) was elaborated, where classesof low, medium, high, very high, and extremely high naturalerosion potential (NEP) were established. Spatial distributionfor the factors R, K, LS, and PNE was defined. The highestaverage R index for the rainy series was 8173.50 MJ ha mm-1h-1 year-1. The period with data from 30 years (1973 – 2002)showed that the reservoir basin displayed areas susceptibleto rill and interill erosion (69.16% of the total). There is apredominance of low erosion potential among the classes,which can be explained due to the soil predominant classesas well as to the low declivity. Areas with medium to extremelyhigh erosion potential require the adoption of measures toavoid start and development of more severe erosion processes(ravines and gullies).
机译:自然潜在的侵蚀是由其主要自然条件在CachoeiraDourada(戈亚斯州和米纳斯吉拉斯州-巴西之间)水文盆地的地区,地理处理技术和全球土壤流失方程(USLE)中定义的。在决定自然侵蚀潜能后,拟定了一个具有侵蚀性(R),可蚀性(K),决定性和斜坡长度(LS)值的矩阵,其中低,中,高,非常高和极高的自然侵蚀潜力类别( NEP)成立。定义了R,K,LS和PNE因子的空间分布。多雨系列的最高平均R指数是8173.50 MJ ha mm-1h-1 year-1。从30年(1973年至2002年)的数据得出的时期表明,该水库盆地显示出易受小溪和层间侵蚀的区域(占总数的69.16%)。这些类别之间的侵蚀潜力很低,这可以解释为土壤占优势的类别以及偏斜率低。具有中等到极高侵蚀潜力的区域需要采取措施,以避免开始和发展更严重的侵蚀过程(沟壑和沟壑)。

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