农业科学与技术(英文版)
農業科學與技術(英文版)
농업과학여기술(영문판)
AGRICULTURAL SCIENCE & TECHNOLOGY
2014年
1期
137-143
,共7页
李雪莹%杨俊%薛忠跃%温海明%王晨雨%程宇%王阳%杨磊
李雪瑩%楊俊%薛忠躍%溫海明%王晨雨%程宇%王暘%楊磊
리설형%양준%설충약%온해명%왕신우%정우%왕양%양뢰
GIS%RUSLE%土壤侵蚀%空间分析%锦州市
GIS%RUSLE%土壤侵蝕%空間分析%錦州市
GIS%RUSLE%토양침식%공간분석%금주시
GIS%RUSLE%Soil erosion%Spatial analysis%Jinzhou City
以 RS和 GIS技术为支撑,利用修正的土壤流失方程(RUSLE)定量评估锦州市2010年水土流失量和土壤侵蚀强度,并对锦州市水土流失空间分布特征进行分析。结果表明,锦州市2010年土壤侵蚀面积为7284.87 km2,占锦州市总面积的70.72%,平均土壤侵蚀模数为18.27 t/(hm2·年),属于轻度侵蚀;15°~25°和6°~15°2个坡度带是研究区土壤侵蚀的主要发生区域。锦州市土壤侵蚀主要发生在农村居民点和旱地2种土地类型,二者的侵蚀量占锦州市2010年总侵蚀量的60.97%。未来应加大对这2种土地类型的治理力度,将其列为水土保持重点治理对象。该研究可为政府制定水土保持的相关政策提供科学依据。
以 RS和 GIS技術為支撐,利用脩正的土壤流失方程(RUSLE)定量評估錦州市2010年水土流失量和土壤侵蝕彊度,併對錦州市水土流失空間分佈特徵進行分析。結果錶明,錦州市2010年土壤侵蝕麵積為7284.87 km2,佔錦州市總麵積的70.72%,平均土壤侵蝕模數為18.27 t/(hm2·年),屬于輕度侵蝕;15°~25°和6°~15°2箇坡度帶是研究區土壤侵蝕的主要髮生區域。錦州市土壤侵蝕主要髮生在農村居民點和旱地2種土地類型,二者的侵蝕量佔錦州市2010年總侵蝕量的60.97%。未來應加大對這2種土地類型的治理力度,將其列為水土保持重點治理對象。該研究可為政府製定水土保持的相關政策提供科學依據。
이 RS화 GIS기술위지탱,이용수정적토양류실방정(RUSLE)정량평고금주시2010년수토류실량화토양침식강도,병대금주시수토류실공간분포특정진행분석。결과표명,금주시2010년토양침식면적위7284.87 km2,점금주시총면적적70.72%,평균토양침식모수위18.27 t/(hm2·년),속우경도침식;15°~25°화6°~15°2개파도대시연구구토양침식적주요발생구역。금주시토양침식주요발생재농촌거민점화한지2충토지류형,이자적침식량점금주시2010년총침식량적60.97%。미래응가대대저2충토지류형적치리력도,장기렬위수토보지중점치리대상。해연구가위정부제정수토보지적상관정책제공과학의거。
Supported by RS technology and GIS technology, the amount of soil loss and soil erosion intensity in Jinzhou City in 2010 were quantitatively evaluated by the modified RUSLE model. The characteristics of the spatial distribution of soil loss in Jinzhou City were analyzed. The results showed that the soil erosion area of Jinzhou City in 2010 was 7 284.87 km2, accounting for 70.72% of the total area of Jinzhou City. The average soil erosion modulus was 18.27 t/(hm2·a), belonging to mild erosion. Two slope belts of 15°-25° and 6°-15° were the main soil erosion re-gions in Jinzhou City. Soil erosion in Jinzhou City was mainly concentrated in the rural residential land and the dry land, and the soil erosion amount of these two land types accounted for 60.97%of the total soil erosion amount in Jinzhou City in 2010. It was suggested that the treatment of these two land types should be strengthened and be main treatment object for soil and water conservation in future. The research could provide scientific basis for the governments to make policies about soil loss.