基于典范对应分析的干旱区春季盐渍化特征研究
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国家自然科学基金项目(40961025,40901163,U1138303/L08)、资源与环境信息系统国家重点实验室开放基金(2010kf0003sa)和新疆维吾尔自治区高校青年教师科研培育基金项目(XJEDU2011S07)


Characterization of soil salinization in arid area based on canonical correspondence analysis
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    摘要:

    运用常规统计学和典范对应分析方法,对干旱区盐渍土土壤全盐量(TS)、盐分离子组成、碱化度(ESP)、pH、电导率(EC)的空间分布特征进行了分析。结果表明,该区土壤为重度至轻度盐化,不同层次土壤中,Na+与Cl-、Ca2+与Mg2+保持较好的关联性。TS的空间分布,在0~50 cm全剖面上主要受控于Cl-、HCO3-和Na+ 离子;分层与全剖面的情况略有不同, Cl-、Na+在各个土层仍为主要控制离子。ESP在全剖面上其空间分布受环境因子的影响较小,0~10 cm土层主要受Na+与Cl-离子的制约;10~30 cm土层内主要受HCO3-离子的制约;30~50 cm土层未表现控制因子。pH在全剖面上受盐分离子的影响较小,分布较为均匀, 表层受离子影响很小,在10~30 cm、30~50 cm土层内受HCO3-离子的影响微弱。EC在全剖面上的空间分布受控于Ca2+、Mg2+离子,30~50 cm土层主要受K+离子的控制,其他土层与全剖面相同。

    Abstract:

    Analysis of characteristics of spatial distributions of total salt content (TS), ion composition, exchangeable sodium percentage (ESP), pH value and electrical conductivity (EC) of salt-affected soils in the Arid Area was conducted, using conventional statistics and canonical correspondence analysis. Results show that (1) the soils in the region are heavily to slightly alkalized, e.g. heavy in topsoil ( 0~10 cm ) and slight in bottom ( 30~50 cm );(2) close correlation exists between Na+ and Cl- , and between Ca2+ and Mg2+ in all soil layers; (3) Cl-, HCO3-and Na+ are the main factors controlling spatial distribution of soil total salt throughout the whole profile ( 0~50 cm ), which though varies slightly from layer to layer, where Na+ and Cl- remain to main factors; (4) the spatial distribution of ESP in the profile is less affected by environmental factors, however, it is restricted mainly by Na+and Cl- in the 0~10 cm soil layer, by HCO3-in the 10~30 cm soil layer, and by none in the 30~50 cm soil layer; (5) pH is quite evenly distributed throughout the profile and only slightly affected by salt ions, that is, it is very slightly affected by ions in the 0~10 cm soil layer, and only weakly influenced by HCO3-in the 10~30 cm and 30~50 cm soil layers; (6) the spatial distribution of EC is controlled by Ca2+ and Mg2+ throughout the whole profile, except in the 30~50 cm soil layer where K+ is the dominant controlling factor.

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韩桂红,塔西甫拉提.特依拜,买买提沙吾提,张 飞.基于典范对应分析的干旱区春季盐渍化特征研究[J].土壤学报,2012,49(4):681-687. DOI:10.11766/trxb201107160261 Han Guihong, Tiyip Tashplat, Mamatsawt, Zhang Fei. Characterization of soil salinization in arid area based on canonical correspondence analysis[J]. Acta Pedologica Sinica,2012,49(4):681-687.

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  • 收稿日期:2011-07-16
  • 最后修改日期:2012-02-16
  • 录用日期:2012-02-23
  • 在线发布日期: 2012-04-23
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