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新安江上游水土流失成因初探
引用本文:洪法水,石树人,王益福.新安江上游水土流失成因初探[J].淮北煤炭师范学院学报(自然科学版),1994(1).
作者姓名:洪法水  石树人  王益福
作者单位:淮北煤师院生物系 (洪法水),安徽大学生物系 (石树人),安徽大学生物系(王益福)
摘    要:作者于八十年代中期实地考察了新安江上游的环境质量。本文对该流域的水土流失程度和形成原因进行了初步探讨。该流域存在有四种形成水土流失的潜在因素即地形地貌特殊,降雨集中且强度大、土垠质地低劣、温差变动幅度大。近三十几年来,该流域水土流失日益加剧,这主要是流域的植被、土垠、水分三个生态因子失去了动态平衡,生态环境遭到了严重的破坏。

关 键 词:新安江上游  水土流失  潜在因素  生态因子

Tenbative Survey of Soil Erosion in the upper Reaches of Xin An River
Hong Fashui.Tenbative Survey of Soil Erosion in the upper Reaches of Xin An River[J].Journal of Huaibei Coal Industry Teachers College(Natural Science edition),1994(1).
Authors:Hong Fashui
Abstract:This paper writers joined activity on estimation of enviro - mentrol guahty in the upper reaches of Xin An River durirng middle 80years. The paper has primary surveyed reason for soil erosion in the upper reaches. There are tour potential facts on soil erosion in the upper reaches, special land shape and lardlooks;close falling wa ter and great intensity; bad soil condition; big temperature: difference size. Recent 30year' s ,soil erosion in the upper reaches is more and more increasingly,three ecoligi cal facts of nature vegetation. Soil and water in the upper reaches have lost balanceecological enviroment has been greatly damaged.
Keywords:upper reaches of Xin An River  soil erosion  ecological facts
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