[1]匡恩俊,中本和夫,刘 峰,等.黑龙江省苏打碱土pH和EC与盐分组成的关系[J].黑龙江农业科学,2011,(05):37-41,54.
　KUANG En-jun,Kazuo Nakamoto,LIU Feng,et al.Relationship of pH，EC and Compostion of Saltof Sodic Soil in Heilongjiang Province[J].HEILONGJIANG AGRICULTURAL SCIENCES,2011,(05):37-41,54.
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黑龙江省苏打碱土pH和EC与盐分组成的关系

《黑龙江农业科学》[ISSN:1002-2767/CN:23-1204/S] 卷: 期数: 2011年05 页码: 37-41,54 栏目: 出版日期: 2011-05-10
Title:
Relationship of pH，EC and Compostion of Saltof Sodic Soil in Heilongjiang Province
文章编号:
1002-2767（2011）05-0037-05
作者:
匡恩俊1; 中本和夫2; 刘 峰3; 迟凤琴1; 矫 江3; 张久明1
1.黑龙江省农业科学院 土壤肥料与环境资源研究所/黑龙江省土壤环境与植物营养重点实验室，黑龙江 哈尔滨 150086；
2.日本国际农林水产研究中心，筑波 305-8686，日本;
3.黑龙江省农业科学院，黑龙江 哈尔滨 150086
Author(s):
KUANG En-jun1; Kazuo Nakamoto2; LIU Feng3; CI Feng-qin1; JIAO Jiang3; ZHANG Jiu-ming1
1.Soil Fertilizer and Environment Resource Institute of Heilongjiang Academy of Agricultural Sciences，Key Lab of Soil Environment and Plant Nutrition of Heilongjiang Province Harbin，Heilongjiang 150086；
2.Japan International Research Center for Agriculture Sciences，Tsukuba 305-8686，Japan;
3.Heilongjiang Academy of Agricultural Sciences，Harbin，Heilongjiang 150086
关键词:
苏打碱土; 地下水位; 离子组成
Keywords:
sodic soil; groundwater; ion composition
分类号:
S151.9
文献标志码:
A
摘要:
通过对比苏打碱土上无植被“碱斑”和临近有植被的“草地”土壤水分、离子变化规律，研究了碱土各种离子及其与土壤pH、EC的关系。结果表明：即使在极端干旱的气象条件下，地下水对地表水补给能力仍然很强，地下水参与土壤盐分运动的现象明显。碱斑土壤pH高于草地；在高水分条件下，pH的峰值出现位置在地表下30 cm，土壤干旱过程，pH峰值位置上移至10～20 cm亚表层内。不同时期EC随土层的加深逐渐降低，且EC的峰值出现在亚表层0～20 cm。碱斑EC值高于草地；土壤pH和EC均与CO32-、SO32-、K+、Na+离子浓度呈显著正相关，而与HCO3-、Cl-、Ca2+、Mg2+相关性不显著。
Abstract:
Comparing the change regularity of soil moisture and ions on no vegetation base spot and vegetation near a grass of sodic soil，the relation of soil pH，EC and the ions were conducted.The result showed that the supply capacity of groundwater to surface water was still strong，the phenomenon of groundwater participating soil salt movement was obvious，even under the extremely draught condition.The pH of base pot was higher than that of grass.In high water condition，peak of pH was in subsurface 30 cm，and when soil drought，peak of pH was in the subsurface between 10～20 cm.EC of different period gradually reduced with soil depth，and the peak of EC was in the subsurface between 0～20 cm.EC value of base pot was higher than that of grass.The pH and EC of soil were significant positive correlation with CO32-，SO42-，K+，Na+ concentration，and had no significant correlation with HCO3-，Cl-，Ca2+，Mg2+ concentration.

参考文献/References:

[1] 王遵亲，祝寿泉，俞仁培等 . 中国盐渍土 [M]. 北京 : 科学出版社， 1993.

[2]龚洪柱.盐碱地造林学[M].北京:中国林业出版社，1988.

[3]罗金明，杨帆，邓伟等.苏打盐渍土的微域特征及土壤表层积盐机理探讨[J].水土保持学报，2008，22（2）：88-92.


备注/Memo

第一作者简介：匡恩俊（1982-），女，黑龙江省海林市人，硕士，研究实习员，从事土壤改良研究。E-mail:kuangenjun2002@163.com。

更新日期/Last Update: 2014-10-31