The spatial variation of physical and chemical properties for eolian sand soil at longitudinal dune scale in southern Gurbantunggut Desert was studied by means of geostatistical methods. In the study, 184 samples of eolian sand soil from the quadrats of 5 m×5 m were systemically collected over the dune crests, slopes and interdune areas of two longitudinal dunes in southern Gurbantunggut Desert and 100 quadrats of vegetation were measured. The physical and chemical properties of eolian sand soil, including soil grain-size parameters, pH, salts, water content, total N and organic matter were determined. The results show that under the impact of longitudinal dune landform characteristics, including elevation, slope aspect, slope angle and partial micro-terrain and vegetation pattern, the physical and chemical properties of eolian sand soil have the variance of weak to medium extent and the spatial autocorrelation of moderate to strong extent. The values of spatial correlated ranges are 21.3-74.8 m, which approximately correspond to a width of single longitudinal dune or a width of landform unit from interdune area to dune to interdune. Because these soil properties have a nest structure of different level systems, the fractal dimensions, D values at different scales were gained. The D values of soil grain-size parameters (φ1, Mz,σ), soil salts (EC) and soil nutrients (organic matter and total N) in a sampling interval of 0-40 m are larger, and the spatial variation is basically medium to high level. Under a sampling interval of 90-150 m, the D values were sharply reduced and the spatial variations were greatly increased. The curve of variation strength for soil water contents was in several segments and the D values were gradually decreased in turn. The mechanism of the close relationship of the spatial variations between soil total N and organic matter contents shows that the spatial variations of the soil physical and chemical properties, which are expressed by the fractal dimensions and not regularly preprocessed, well accord with the field facts.
[1] 王政权, 王庆成. 森林土壤物理性质的空间异质性研究. 生态学报, 2000, 20(6): 945~950.
[2] Burgess T M, Webster R. Optimal interpolation and isarithmic mapping of soil propertiesⅠ:The semivariogram and punctual Kriging. Journal of Soil Science, 1980, 31: 315~331.
[3] 马风云, 李新荣, 张景光, 等. 沙坡头固沙植被若干土壤物理因子的空间异质性研究. 中国沙漠, 2005, 25(2): 208~215.
[4] 王红, 宫鹏, 刘高焕. 黄河三角洲多尺度土壤盐分的空间分异. 地理研究, 2006, 25(4): 649~658.
[5] Legendre P, Fortin M J. Spatial pattern and ecological analysis. Vegetation, 1989, 80: 107~138.
[6] Goovaerts P. Geostatistical tools for characterizing the spatial variability of microbiological and physico-chemical soil properties. Biology and Fertility of Soils, 1998, 27: 315~334.
[7] 姜秋香, 付强, 王子龙. 空间变异理论在土壤特性分析中的应用研究进展.水土保持研究, 2007, 14(4): 413~419.
[8] Frank S G, David A D. Spatial heterogeneity of soil nutrients and plant species in herb-dominated communities of contrasting land use. Plant Ecology, 2010, 209: 83~94.
[9] 杨兆平, 欧阳华, 徐兴良, 等. 五道梁高寒草原土壤水分和植被盖度空间异质性的地统计分析. 自然资源学报, 2010, 25(3): 426~434.
[10] 张宁, 滕玖琳, 何兴东, 等. 猫头刺群落对土壤养分空间异质性的响应. 中国沙漠, 2008, 28(4): 706~711.
[11] 钱亦兵, 吴兆宁, 杨海峰, 等.古尔班通古特沙漠南部风沙土粒度分布的空间异质性. 干旱区地理, 2009, 32(5): 655~661.
[12] 钱亦兵, 吴兆宁, 杨海峰, 等. 古尔班通古特沙漠纵向沙垄植被空间异质性. 中国沙漠, 2011, 31(2): 420~429.
[13] Fork R L, Ward W C. Brazos river bar: A study in the significance of grain size parameters. Journal of Sedimentary Petrology, 1957, (27): 3~26
[14] 任明达, 王乃梁. 现代沉积环境概论. 北京: 科学出版社. 1981. 8~9, 14.
[15] 杨海峰, 钱亦兵, 蒋超, 等. 古尔班通古特沙漠南缘主要土壤化学特征的空间异质性. 中国沙漠, 2010, 30(2): 319~325.
[16] Qian Y B, Wu Z N, Zhao R F, et al. Vegetation patterns and species-environment relationships in the Gurbantunggut Desert of China. Journal of Geographical Sciences, 2008, 18(4): 400~414.
[17] 蒋超, 钱亦兵, 杨海峰, 等.古尔班通古特沙漠南缘浅层风沙土含水量的空间变异.干旱区研究, 2009, 26(4): 519~525.
[18] 王政权. 地统计学在生态学中的应用. 北京: 科学出版社, 1999. 3~4, 65~100.
[19] 尚占环, 姚爱兴, 龙瑞军. 干旱山地生态系统植物群落不同尺度下物种数的变化特征. 干旱区地理, 2005, 28(6): 805~810.
[20] 胡旭, 王海涛, 卢建国, 等. 干旱和半干旱区油蒿对土壤空间异质性的响应. 中国沙漠, 2007, 27(4): 587~592.
[21] 阿如旱, 杨持, 同丽嘎. 基于分形理论的沙漠化土地空间结构--以内蒙古多伦县为例. 地理研究, 2010, 29(2): 283~290.
[22] Cambardella C A, Moorman T B, Novak J M, et al. Field-scale variability of soil properties in central Iowa Soils. Soil Science Society America Journal, 1994, 58(5): 1501~1511.
[23] 何志斌, 赵文智. 黑河下游荒漠河岸林典型样带植被空间异质性. 冰川冻土, 2003, 25(5): 591~596.
[24] Chen Y F, Yu F H, Dong M. Scale-dependent spatial heterogeneity of vegetation in Mu Us sandy land, a semi-arid area of China. Plant Ecology, 2002, 162: 135~142.
[25] 辛晓平, 李向林, 杨桂霞, 等.放牧和刈割条件下草山草坡群落空间异质性分析. 应用生态学报, 2002, 13(4): 449~453.
[26] 张华良, 刘振义, 刘朝杰. 数学地质. 北京: 冶金工业出版社, 1994. 210.
[27] 潘颜霞, 王新平. 荒漠人工植被区浅层土壤水分空间变化特征分析. 中国沙漠, 2007, 27(2): 250~256.
[28] 刘继龙, 马孝义, 张振华. 土壤水盐空间异质性及尺度效应的多重分形. 农业工程学报, 2010, 26(1): 81~86.
[29] 张继光, 陈洪松, 苏以荣, 等. 喀斯特洼地表层土壤水分的空间异质性及其尺度效应. 土壤学报, 2008, 45(3): 544~549.
[30] 郑敬刚, 张本昀, 何明珠, 等. 灌丛化对贺兰山西坡草场土壤异质性的影响. 干旱区研究, 2009, 26(1): 27~31.
[31] 张华, 何红, 李锋瑞, 等. 科尔沁沙地灌木对风沙土壤的生态效应. 地理研究, 2005, 24(5): 708~716.
[32] 李元寿, 张人禾, 王根绪, 等. 青藏高原典型高寒草甸区土壤有机碳氮的变异特征. 环境科学, 2009, 30(6): 1826~1831.
[33] 王军, 傅伯杰, 邱扬, 等. 黄土高原小流域土壤养分的空间分布格局--Kriging插值分析. 地理研究, 2003, 22(3): 373~379.