以贵州喀斯特地区的王家寨小流域为研究对象,基于多源信息,依托RS和GIS技术获取2005年该流域石漠化景观格局信息,以此为基础进行石漠化景观分布指数、石漠化综合指数、 -s平面分析模型以及三次曲线拟合等分析,旨在从小流域尺度上探讨石漠化景观在坡度、坡向、高程和与村庄距离等空间因子上的分布规律。结果表明:潜在、轻度石漠化景观受坡度影响最显著;其他类型石漠化景观受坡向影响最明显。石漠化程度先随坡度的增大而加重,27°后呈缓解趋势;各坡向中南、东南坡石漠化最严重;随高程增加石漠化加剧;距村庄越远石漠化越严重。初步推断各空间因子对石漠化程度的影响由强至弱的顺序为:坡度、坡向、高程、与村庄的距离。

The impact of spatial factors on karst rocky desertification landscape was studied in Wangjiazhai catchment.Based on the image of SPOT5 in 2005, with the support of the geographic information system (GIS) and remote sensing (RS) software, karst rocky desertification landscape patterns in the studied area was classified as: no, latent, slight, moderate, strong, and extremely strong karst rocky desertification types. Meanwhile, four spatial factors (slope, slope aspect, elevation and distance to the village) were derived from the digital elevation model. Quasi-quantitative analysis was made on the relationships between the above four factors with karst rocky desertification landscape distribution index (RLDI) and karst rocky desertification comprehensive index (RCI), respectively. Results indicate that: (1)The distribution of various rocky desertification landscapes along the spatial gradient is different. For example, the latent and slight rocky desertification is affected by slope aspect more greatly than that on other spatial factors; while the moderate, strong and extremely strong rocky desertification is highly correlated with the slope gradient. (2)The four spatial factors affect rocky desertification in different ways. For example, 27° is a critical angle for rocky desertification intensity which becomes severer firstly, and then becomes slighter around the turning point. As to the effects of slope aspect, due to the aspect of terrane and exogenic forces including solar radiation and precipitation, the severest rocky desertification occurs in regions of south or southeast slope aspect; and less for north, northeast and east cases, while it is slight in other cases. Moreover, with the increase of elevation, the intensity of rocky desertification is in a deteriorative trend. The regulation of rocky desertification along the distance to the village reveals the mode of human activities on rocky desertification process. (3) The fittings between RCI values and four factors, using the cubic curve estimation method, are obviously different in the descending order: slope>slope aspects>elevation>the distance to the village. The order, in a sense, shows the intensities of those spatial factors on RCI values. Though influences of each spatial factor on RCI could be evaluated by using single-factor correlation analysis, it also should notice that those factors affected RCI mutually.