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[1]ZHANG Fei,Tashpolat·Tiyip,DING Jian-li,et al.Application of Salt Distribution Chemical Field Theory in Soil Salination in Arid Oasis—A Case Study in the Delta Oasis Of Weigan and Kuqa Rivers[J].Research of Soil and Water Conservation,2008,15(04):88-93,97.

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Application of Salt Distribution Chemical Field Theory in Soil Salination in Arid Oasis—A Case Study in the Delta Oasis Of Weigan and Kuqa Rivers

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 15 Number of periods: 2008 04 Page number: 88-93,97 Column: Public date: 2008-08-20

Title:: Application of Salt Distribution Chemical Field Theory in Soil Salination in Arid Oasis—A Case Study in the Delta Oasis Of Weigan and Kuqa Rivers

Author(s):: ZHANG Fei^1,2, Tashpolat·Tiyip¹, DING Jian-li¹, HE Qi-sheng³; 1. R & E Department of Xinjiang University, Key Laboratory of Oasis Ecology, Xinjiang University, Ministry of Education, Urumqi 830046, China;
2. Graduate school of Xinjiang University with Academic Degrees Committee, Urumqi 830046, China

Keywords:: the delta oasis of Weigan and Kuqa rivers; salinization; salt distribution field in water-soil environment; variogram function

CLC:: S156.4

DOI:: -

Abstract:: In this paper,author has proposed the delta oasis of Weigan and Kuqa rivers which are located in the North of Tarim Basin considered as the typical area. According to regional distribution characteristics of salt in water-soil environment,the theories of Salt Distribution Field in water-soil Environment are applied. Variation function offered is used to model quantitatively space differentiation of salt in water-soil environment,thus,the Geostatistics is used in soil science to explore its spatial distribution characteristics and its variability law,which has been advocated by more and more experts. The fundamental of geostatistics and its utilization in soil spatial variability on soil physical characteristics,soil conductivity and salt content were reviewed in this paper. Geostatistics combined with GIS was applied to analyze the spatial variability of soil conductivity and salt content in topsoil in the delta oasis of Weigan-Kuqa rivers. In this paper,the research which was based on Kriging method,was handled by ArcGIS. GIS can integrate attribute data with geographical data of system variables,which makes the application of geostatistics technique for large spatial scale more convenient. It is showed that the spatial correlation of topsoil conductivity and salt content at this large scale were strongly dependent,the proportion of Nugget and Sill is 44.72% and 38.61%. Variance coefficient is 0.634 and 0.618. Then choosing proper Kriging model,verifying of the Cross-Validation and correcting the parameters are important factors influencing accurate analysis. At last,this method is applied by integrating experimental data in saline soil of the delta oasis of Weigan and Kuqa rivers,and get EC,salt content sample in saline badlands,at the same time,get different direction EC,salt content sample variance. This theories can be used quantificationally study on saline and alkaline water-soil environment.

References:: [1] 史海滨, 陈亚新, 朝伦巴根, 等.表土盐分空间变异及合理采样与信息估计[J].内蒙古农牧学院学报, 1996, 17(4):74-81.
[2] 宋长春, 闫百兴, 宋新山.电磁技术在苏打盐渍化土壤研究中的应用[J].地理科学, 2002, 22(1):91-95.
[3] 李取生, 王志春, 李秀军.苏打盐渍土壤微咸水淋洗改良技术研究[J].地理科学, 2002, 22(3):342-348.
[4] 沈思渊.土壤空间变异性:事实, 调节和应用[J].国外农学:土壤肥料, 1988(2):35-42.
[5] 沈思渊.土壤空间变异研究中地统计学的应用及其展望[J].土壤研究进展, 1989(2):11-25.
[6] 王德利.植物生态场导论[M].长春:吉林科学技术出版社, 1994.
[7] 王亚秋, 王德利.改进的植物生态场模型与实例分析[J].生态学报, 2005, 25(11):2855-2861.
[8] 汪林, 汪珊, 甘泓, 等.宁夏青铜峡灌区水土化学场演化态势初步分析[J].水利学报, 2003(6):78-84.
[9] 李海涛, 李小梅, Philip B, 等.电磁感应方法在土壤盐渍化评价中的应用研究[J].水文地质工程地质, 2006, 33(1):95-98.
[10] 钱云, 郝毓灵.新疆绿洲[M].乌鲁木齐:新疆人民出版社, 2000:358-359.
[11] 周福俊, 单润起, 张中庸.松嫩平原中部地区地下水化学研究[M].长春:吉林大学出版社, 1994:168.
[12] 钱贞国.松嫩平原西部盐碱湿地开垦前后水土环境化学特征变化[D].长春:中国科学院长春地理所, 1997:20.
[13] 王政权.地统计学及其在生态学中的应用[M].北京:科学出版社, 1999:1-5, 177-185.
[14] Kemper W D, Van Schaik J C. Distribution of salt in soil water systems[J]. Soil Sci. Soc. Am. Proc., 1966, 30(5):534-538.
[15] Guitjens J C. Spatial and temporal variabilities in salinity[C]//Tanji K K. Agricultural salinity assessment and management. New York: American Society of Civil Engineers, 1990:328.
[16] Webster R. Quantitative spatial analysis of soil in the field[J].Advances in soil science, 1985, 3:1-4.
[17] 祝寿泉.我国土壤盐渍化的发生及演变[C]//俞仁培, 郭建新, 胡祥明.全国盐渍土研究学术研讨会会议论文集:盐渍土资源综合开发利用与治理.中国土壤学会盐渍土专业委员会, 1997:25.
[18] 朱发庆.环境规划[M].武汉:武汉大学出版社, 1994:85-90, 203-210.
[19] Matheron G. The theory of regionalized variables and its applications[M]. Cahiers Du Centre De Morphlogie Mathematique, Fontainblean, 1971:56.
[20] 华孟, 王坚.土壤物理学[M].北京:北京农业大学出版社, 1993:214-237.
[21] Alemi M H, Azari A B, Nielsen D R. Kriging and univariate modeling of a spatial correlated data[J]. Soil Technology, 1989, 1(2):133-147.
[22] 徐吉炎, 韦甫斯特.土壤调查数据地域统计的最佳估值研究[J].土壤学报, 1983, 20(4):419-430.
[23] 李哈滨, 王政权, 王庆成.空间异质性定量研究理论与方法[J].应用生态学报, 1998, 9(6):651-657.
[24] 姚荣江, 杨劲松, 刘广明, 等.黄河三角洲地区典型地块土壤盐分空间变异特征研究[J].农业工程学报, 2006, 22(6):61-66.
[25] 胡克林, 余艳, 张凤荣, 等.北京郊区土壤有机质含量的时空变异及其影响因素[J].中国农业科学, 2006, 39(4):764-771.
[26] 李军, 游松财, 黄敬峰.中国1961-2000年月平均气温空间插值方法与空间分布[J].生态环境, 2006, 15(1):109-114.
[27] 胡克林, 张凤荣, 吕贻忠, 等.北京市大兴区土壤重金属含量的空间分布特征[J].环境科学学报, 2004, 24(3):463-468.
[28] Cambardella C A, Moorman T B, Novak J M, et al. Field-scale variability of soil properties in central low a soils[J].Soil Sci Soc Am.J., 1994, 58:1501-1511.
[29] Zhang S R, Sun B, Zhao Q G, et al. Temporal-spatial variability of soil organic carbon stocks in rehabilitating ecosystem[J], Pedosphere, 2004, 14(4):501-508.
[30] Chien Y J, Lee D, Guo H Y, et al.Geostatistics analysis of soil properties of mid-west Taiwan soils[J].Soil Sci., 1997, 162:291-298.
[31] 叶海燕, 王永平, 王金栋, 等.渭干河灌区水盐均衡特征分析[J].农业工程学报, 2003, 19(4):92-96.

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