喀斯特地区典型洼地土壤水分的垂直变异性研究
Vertical variability of soil moisture content in the representative depression areas of karst region
利用2005年5月在桂西北喀斯特洼地10m×10m地块范围内的网格 (2m×2m) 采样数据,用地统计学方法分析了两种土地利用类型(玉米地和牧草地)0~80cm土壤水分的垂直变异结构及其分布格局。结果表明:玉米地和牧草地土壤水分呈现弱变异特征,两者的垂直变异趋势大致随土层加深先减小后增大,其中牧草地土壤水分的变异程度相对较大;玉米地和牧草地土壤水分在垂直层面均具有良好的半方差结构和较强的空间相关性,都可用球状模型拟合,变程分别是66.0cm和49.1cm。垂直变异还具有明显的各向异性,均可用指数模型拟合;土壤水分的空间相关性及变程与土壤容重具有一定关系,而且研究显示洼地退耕还草后土壤总体上朝着有利于水分保蓄和植被恢复的方向转变。
In the karst depression areas at northwest Guangxi, grid sampling method was adopted (2m×2m) in a square area (10m×10m), and soil moisture content at 0~80㎝ soil depth by 10㎝ interval within two land use types was measured in may 2005. The vertical variability construction and distributing pattern were analyzed by the Geo-statistics method. The results showed that the corn land and the grassland possessed weak variability. Their vertical variability decreased and then increased along with soil layers but the grassland bad bigger spatial variability, The corn land and the grassland both had good semi-variance structure and strong spatial correlation, and they could be well expressed by spherical model. And their range were 66㎝ and 49.1㎝ respectively. They both had obvious anisotropy in vertical soil layers and could be fit with exponential model. The research also found that the spatial correlation and range of soil moisture have relationship with soil bulk density in this area. And it can help to maintain soil moisture and promote vegetation restoration in the depression areas after the “grain-for-green”.
张继光、张伟、苏以荣、陈洪松
农业科学研究
土壤水分 喀斯特 垂直变异 半方差
soil moisturekarstvertical variabilitysemi-variance
张继光,张伟,苏以荣,陈洪松.喀斯特地区典型洼地土壤水分的垂直变异性研究[EB/OL].(2006-09-15)[2025-08-03].http://www.paper.edu.cn/releasepaper/content/200609-241.点此复制
评论