Knowledge Resource Center for Ecological Environment in Arid Area
盐分对极干旱土壤水分垂直分布与运转的影响 | |
其他题名 | Salinity Influence on Soil Moisture Vertical Distribution and Transport in Extremely Dry Area |
李红寿; 汪万福; 武发思; 安黎哲 | |
来源期刊 | 土壤
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ISSN | 0253-9829 |
出版年 | 2011 |
卷号 | 43期号:5页码:809-816 |
中文摘要 | 通过对莫高窟戈壁土壤中主要盐分的检测和理化特性分析,发现在极干旱地区,土壤盐分对土壤水分的垂直分布产生了重要影响。以芒硝为代表的结晶盐分,其含量分布和理化特性与土壤水分分布非常吻合。0~20cm以无水盐分(Na_2SO_4)为主,水分含量较低,是盐分集聚层;在20~50cm以结晶盐分(Na_2SO_4·10H_2O)为主,水分含量较高,是盐分析出层;50cm以下以膜状水盐溶液为主,水分含量较低。与附近含盐量较低的流沙相比,盐分使戈壁土壤的水分含量增大了10倍以上,在热动力学作用下使浅层土壤水分的活动能力大大增强,对GSPC系统水分的垂直运转和潜水蒸发产生了重要影响。这为极干旱区利用潜水进行生态恢复提供了新的可能,对莫高窟的文物保护也具有重要意义。 |
英文摘要 | Through measuring and analyzing salinities'physical and chemical characteristics of Gobi soil near the Mogao Grottoes, we discovered that soil salinity had a great impact on the vertical distribution of soil water content.The content distribution, physical and chemical characteristics of crystal salinities, which was represented by mirabilite, tallied closely with the distribution of soil moisture.The depth from 0 to 20 cm was mainly dominated by anhydrous salinities(Na_2SO_4), and water content was relatively low, it was salt concentration layer.The depth from 20 to 50 cm was mainly dominated by crystal salinities(Na_2SO_4·10H_2O), and water content was relatively high, it was salt precipitation layer.The depth of below 50 cm was mainly dominated by filmy salt solution, and water content was relatively low.Compared with near dune which had low salinity, salinity caused water content of Gobi soil increased by 10 times more.Under thermokinetics action, water movement was greatly increased in shallow soil.It is important to the upright water transport and ground water evaporation of GSPAC system.This offers a new way to ecological recovery by using ground water and also important to protect Mogao grottoes cultural relics. |
中文关键词 | 盐分 ; 土壤水分 ; 芒硝 ; 极干旱地区 |
英文关键词 | Salinity Soil moisture Mirabilite Extremely dry area |
类型 | Article |
语种 | 中文 |
收录类别 | CSCD |
WOS类目 | Agriculture |
CSCD记录号 | CSCD:4347295 |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/378726 |
作者单位 | 李红寿, 敦煌研究院保护所, 敦煌, 甘肃 736200, 中国.; 汪万福, 敦煌研究院保护所, 敦煌, 甘肃 736200, 中国.; 武发思, 敦煌研究院保护所, 敦煌, 甘肃 736200, 中国.; 安黎哲, 兰州大学生命科学学院, 兰州, 甘肃 730000, 中国. |
推荐引用方式 GB/T 7714 | 李红寿,汪万福,武发思,等. 盐分对极干旱土壤水分垂直分布与运转的影响[J],2011,43(5):809-816. |
APA | 李红寿,汪万福,武发思,&安黎哲.(2011).盐分对极干旱土壤水分垂直分布与运转的影响.土壤,43(5),809-816. |
MLA | 李红寿,et al."盐分对极干旱土壤水分垂直分布与运转的影响".土壤 43.5(2011):809-816. |
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