干旱区生态环境知识资源中心(Arid): 中国耕地土壤侵蚀空间分布特征及生态背景

Arid

	中国耕地土壤侵蚀空间分布特征及生态背景
其他题名	The Soil Erosion Distribution Characteristics and Ecological Background of Chinese Cultivated Land
	田光进; 张增祥; 赵晓丽; 张国平; 谭文彬
来源期刊	生态学报
ISSN	1000-0933
出版年	2002
卷号	22 期号:1 页码:10-16
中文摘要	利用20世纪90年代中期全国土壤侵蚀遥感调查数据和耕地数据分析了全国耕地侵蚀情况。20世纪90年代中期全国耕地受土壤侵蚀面积占33.15%。水力侵蚀面积较大，占耕地土壤侵蚀面积的88.43%，风力侵蚀占11.08%，冻融侵蚀占0.32%，重力侵蚀占0.04%，工程侵蚀占0.13%。土壤侵蚀以旱地为主，水田较少。旱地水力侵蚀中较为严重的地区主要分布在黄土高原、云贵高原、四川及南方丘陵地区，风力侵蚀主要分布在西北和东北地区。水田受水力侵蚀分布在西南地区，水田受力侵蚀主要分布在黑龙江、辽宁等地区。冻融侵蚀主要分布在内蒙古、青藏高原等地区，广东省的工程侵蚀和重力侵蚀较为严重。还分析了旱地水力侵蚀与地形、植被和降雨量等生态背景的关系，利用生态环境综合指数和土壤侵蚀强度指数分析了土壤侵蚀与生态背景的关系，当生态环境综合指数≤4.33时，生态背景综合指数与土壤侵蚀强度具有很强的相关性。
英文摘要	China is country with vast population and scarce cultivated land per capita. About 33% of the arable land was eroded by wind、Water、frost、gravitation and engineering forces. In order to investigate the soil erosion condition and protection measures of the cultivated lsand the soil erosion survey was one by intepretating TM imagery of 1995 and 1996 in China. Landsat TM imagery was composed, projected, rectified and interpreted to get the 1 : 100000 vector data of the national land use and the soil erosion map with the help of field investigation, topography, vegetation, soil quality, and soil erosion map. The provincial maps were collected into the national ones. The soil erosion was classified into water erosion, wind erosion, frost erosion, gravitation erosion and engineering erosion in terms of the national standard issued in 1996. The soil erosion intensity was classified into six grades. About 75.05% of Chinese cultivated land was dry hand and 24.95% was paddy field. The soil erosion of the dry land was more serious than that of the paddy field. About 42.48% of the dry land was eroded while 7.96% of the paddy field was eroded. Totally, 33.15% of the cultivated land was eroded. The water force erosion took up 88.43% of all the eroded cultivated land and the wind erosion was about 11.08%. The eroded cultivated land by water forces was mainly located in Sichuan, Heilongjiang, Gansu, Shaanxi, Inner Mongolia, Yunnan, Shanxi, Guizhou and Chongqing. They concentrated in the Loess plateau, Yungui plateau and Sichuan mountain area. In Chongqing municipality, Guizhou, Sichan and Gansu Provinces the eroded percentage was more than 80%. That of Shaanxi, Yunnan, Ningxia, Inner Mongolia, Fujian and Shanxi was more than 51%. The water eroded dry land in Heilongjiang took up about 38.14% of that of Chinese cultivated land because its dry land was large. The highly serious water erosion located mainly in Loess plateau and Yunan, Guizhou, Sichuan, Fujian and Jiangxi mountain area. The acreage of the wind eroded dry land was located in Inner Mongolia, Jilin, Heilongjiang, Hebei, Henan, Xinjiang and Gansu Provinces which took up about 91.66% of the national wind erosion. Inner Mongolia was the most serious area by the wind erosion and the eroded percentage was more than 36.1%. The percentage of Jilin、Ningxia、Xinjiang and Hebei Provinces was more than 7%. More mountain and hill areas were distributed in Sichuan, Yunnan, Guizhou, Anhui, Heilongjiang, Guangxi, Hubei and Zhejiang and were the main water erosion areas in China. The water eroded paddy field was more than 10% in Yunnan, Guizhou and Sichuan Provinces. The wind eroded paddy field in Heilongjiang took up about 55.12% and Liaoning was 9.2%, Hubei 7.83%, Jilin 7.35%, Inner Mongolia 6.52%. The wind eroded areas were located in Northern China. In Inner Mongolia the wind eroded paddy field was about 9.12. The frost erosion happened in the coldest areas including Inner Mongolia, Tibet and Qinghai which took up about 82.77%、16.76% and 0.34% of Chinese frost erosion acreage respectively. Engineering erosion was caused by mining, quarrying, building and other activities. The engineering erosion in dry land was the most serious in Guangdong Province whose percentage took up 58,01% and Heilongjiang was 14.21%. The engineering erosion in paddy field in Guangdong was about 59.29% of China and Fujian was 15.39%. a great amount of cultivated land was converted into urban、rural settlements and the construction land. The engineering erosion extended without agricultural field protection measurements. The gravitation in Guangdong was most serious with the rapid development of cities. In Chongqing municipality and Hunan Province the slope cultivated land caused the gravitation erosion. From above we could draw the conclusion that the dry land of the water erosion was most serious in China. There was a strong relationship between the soil erosion and the ecological background. In order to study the relationship, SEI (Soil Erosion Intensity Index) and EI (Ecological Environmental Index) were built. EI included slope, precipitation and the vegetation factors. The slope was divided into 6 grades. There was a strong relevance between the slope and the soil erosion intensity index. The higher the slope was, the higher the soil erosion intensity was. NDVI (Normalized Difference Vegetation Index) was gotten by the NOAA data to represent the vegetation condition and was classified into 8 grades. The higher the grade, the better the vegetation. When the NDVI was 3,SEI was the highest; when the vegetation was 2、8、4、7, the SEI was the second; when the vegetation index was 1 where the climate was dry and the precipitation was the lowest, SEI was the lowest. The precipitation was divided into 6 grades by the agricultural climate zoning standard. SEI was the highest when the precipitation was 1000 ～ 1600 mm where was humid. SEI was second in the territory where it was half-humid and the precipitation was 400 ～ 800 mm. SEI was the third when the climate was half-arid and the precipitation was 250 ～ 400 mm. The soil erosion intensity was the lowest in the place where the grade of the precipitation was 4、6 and 1. The soil erosion intensity was affected by the combination of the topography、vegetation、soil quality and precipitation. When EI was ≤ 4.33, the relationship between the ecological factors and the soil erosion intensity was highly relevant. The higher the ecological index, i.e. the slope was higher, the vegetation was worse and the precipitation was less, the more serious the soil erosion intensity. When the ecological index was >4.33, the relevance was not high and the soil erosion intensity was more affected by the single ecological factor.
中文关键词	耕地 ; 土壤侵蚀 ; 空间分布特征 ; 生态环境综合指数 ; 土壤侵蚀强度指数
英文关键词	cultivated land soil erosion spatial distribution charateristics soil erosion intensity index ecological environmental index
语种	中文
国家	中国
收录类别	CSCD
WOS类目	ECOLOGY
WOS研究方向	Environmental Sciences & Ecology
CSCD记录号	CSCD:1067483
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/203373
作者单位	中国科学院遥感应用研究所, 北京 100101, 中国
推荐引用方式 GB/T 7714	田光进,张增祥,赵晓丽,等. 中国耕地土壤侵蚀空间分布特征及生态背景[J],2002,22(1):10-16.
APA	田光进,张增祥,赵晓丽,张国平,&谭文彬.(2002).中国耕地土壤侵蚀空间分布特征及生态背景.生态学报,22(1),10-16.
MLA	田光进,et al."中国耕地土壤侵蚀空间分布特征及生态背景".生态学报 22.1(2002):10-16.