中文摘要：

研究了喀斯特地区典型坡地3条人工开挖样沟（投影长21 m、宽1 m）的岩土结构特征、土壤剖面平均含水量和土岩界面含水量沿坡面向下的变化趋势,探讨了喀斯特坡地基岩起伏对土壤水分格局的影响.结果表明：喀斯特坡地地表地形与基岩地形不一致,基岩深度变异系数最大为82%,基岩起伏较大.基岩起伏程度明显影响到土壤剖面水分分布格局：基岩起伏较小时,土壤含水量呈上坡位至下坡位逐渐增加的趋势,且土壤剖面平均含水量和土岩界面含水量与基岩深度相关性均不显著;基岩起伏越大,土壤含水量沿坡向下线性增加的趋势越不明显,土壤水分空间连续性越差,基岩凹陷、裂隙处土壤含水量较高,土壤剖面平均含水量和土岩界面含水量与基岩深度呈极显著正相关,但后者对基岩起伏的响应更明显.

英文摘要：

Based on three manually excavated trenches（ projection length of 21 m,width of 1 m）along a typical Karst hillslope,the changing trends for soil-bedrock structure,average water content of soil profile and soil-bedrock interface water content along each individual trench were studied.The effect of irregular bedrock topography on soil moisture distribution was discussed. The results showed that the surface topography was inconsistent with the bedrock topography in the Karst hillslopes. The bedrock topography was highly irregular with a maximum variation coefficient of 82%.The distribution pattern of soil profile of moisture was significantly affected by the underlying undulant bedrock. The soil water content was related to slope position when the fluctuation was gentle,and displayed a linear increase from upslope to downslope. When the bedrock fluctuation increased,the downslope linear increasing trend for soil water content became unapparent,and the spatial continuity of soil moisture was weakened. The soil moisture was converged in rock dents and cracks.The average water content of soil profile was significantly positively correlated with the soil-bedrock interface water content,while the latter responded more sensitively to the bedrock fluctuation.