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Land use change and gully erosion in the Piedmont region of South Carolina

机译:南卡罗来纳州皮埃蒙特地区的土地利用变化和沟壑侵蚀

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Land use change played an important role in the formation of gullies present today in the Piedmont of the Southeastern United States. Forested areas that were once cleared to cultivate cotton and consequently gullied are now, once again, covered with forest vegetation. Despite this forest cover, gullies are still considered to be important contributors of sediment to streams, and restoration efforts are still ongoing. However, the data available to assess the extent of gully contributions of sediment are limited.This study assessed the present day stability of these gullies relative to the land use conditions from 1939 to 1999. Based on 1939, 1954, 1970, and 1999 aerial photographs, land areas were classified into those found to be open or cultivated in 1939 that had converted to forest by 1999 (cultivated-to-forested) versus areas that were forested throughout this period (continually forested). An analysis was then conducted that quantified the number and morphological characteristics of gullies in these areas. Characteristics assessed during the field surveys that quantified the presence of recent erosion, such as percent bare soil or forest floor displacement, revealed that the majority of the gullies in both areas are stable. Surprisingly, more frequent (4 vs. 2 per transect), deeper (54 vs. 46 cm), and longer (36 vs. 30 m) gullies were found in the continually forested areas. This equated to a higher estimated average total volume eroded in the continually forested areas (299 m~3) compared to the cultivated-to-forested areas (107 m~3). It is believed that the continually forested areas, which had steeper average slopes, were cultivated but abandoned prior to 1939 due to severe gully formation.
机译:土地用途的变化在当今美国东南部的皮埃蒙特形成的沟渠中起着重要作用。曾经被清理过以种植棉花并因此被开垦的林区现在再次被森林植被覆盖。尽管有这样的森林覆盖,但沟壑仍然被认为是河流中沉积物的重要贡献者,恢复工作仍在进行中。但是,可用于评估沉积物的沟壑贡献程度的数据是有限的。本研究评估了这些沟壑相对于1939年至1999年的土地利用状况的当前稳定性。基于1939年,1954年,1970年和1999年的航拍照片,将土地面积分类为1939年被发现为开放或耕种的土地面积,到1999年已转变为森林(从耕种到森林),而整个时期的森林面积(一直为森林)。然后进行了分析,以量化这些区域中的沟壑的数量和形态特征。在实地调查中评估的特征量化了近期侵蚀的存在,例如裸露土壤的百分比或林地位移,表明这两个地区的大多数沟壑都是稳定的。出人意料的是,在森林覆盖率较高的地区发现沟渠的频率更高(每个横断面4对2),更深(54对46 cm)和更长(36对30 m)。这意味着与耕地到森林的地区(107 m〜3)相比,连续森林地区(299 m〜3)的平均估计总侵蚀量更高。可以认为,由于坡度严重,在1939年之前已耕种但平均坡度较高的连续森林地区。

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