| 黄土丘陵区不同植被土壤水分的分异性特征 |
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| 引用本文： | 刘庚,牛俊杰,朱炜歆,史建伟,梁海斌.黄土丘陵区不同植被土壤水分的分异性特征[J].水土保持通报,2014(6):83-88. |
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| 作者姓名： | 刘庚 牛俊杰 朱炜歆 史建伟 梁海斌 |
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| 作者单位： | 太原师范学院 汾河流域科学发展研究中心, 山西 太原 030012;太原师范学院 汾河流域科学发展研究中心, 山西 太原 030012;太原师范学院 汾河流域科学发展研究中心, 山西 太原 030012;山西大学 黄土高原研究所, 山西 太原 030006;山西大学 黄土高原研究所, 山西 太原 030006 |
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| 基金项目： | 国家自然科学基金项目"晋西北生态重建优势种林地土壤水分研究:以沙棘和柠条为例"(41171423),"顾及污染物向异性特征的土壤有机污染物三维空间分布预测方法研究"(41401236) |
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| 摘 要： | 为定量研究半干旱黄土丘陵区不同植被深层土壤水分的时空分异性特征,选择晋西北岢岚县为目标研究区域,对撂荒地、柠条林、小叶杨林3种林型4—7月份0—600cm深度剖面土壤水分的时空异质性特征进行了分析。研究结果表明:(1)3种植被4个月份内土壤含水量变化范围在3.34%~17.19%之间。在0—200cm深度土壤含水量变化没有明显规律,在200—600cm深度土层范围内,撂荒地、柠条林土壤含水量分别有升高和轻缓降低趋势,小叶杨林有先轻缓降低再轻缓升高趋势。(2)土壤含水量在4个月份间均存在显著性差异(p0.01),不同月份不同植被类型土壤含水量总体分布差异性也都不同。(3)土壤含水量变异系数值大多集中在0~30%之间,个别土层深度变异系数值超过50%,表明土壤水含量总体上具有结构稳定性,但存在局部较强变异特征。
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| 关 键 词： | 土壤水分 黄土丘陵区 空间异质性 生态重建 |
| 收稿时间： | 1/3/2014 12:00:00 AM |
| 修稿时间： | 2014/3/23 0:00:00 |
Heterogeneous Characteristics of Soil Moisture of Different Vegetation Types in Loess Hilly Regions |
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| LIU Geng,NIU Jun-jie,ZHU Wei-xin,SHI Jian-wei and LIANG Hai-bin.Heterogeneous Characteristics of Soil Moisture of Different Vegetation Types in Loess Hilly Regions[J].Bulletin of Soil and Water Conservation,2014(6):83-88. |
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| Authors: | LIU Geng NIU Jun-jie ZHU Wei-xin SHI Jian-wei and LIANG Hai-bin |
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| Institution: | Research Center for Scientific Development in Fenhe River Valley, Taiyuan Normal University, Taiyuan, Shanxi 030012, China;Research Center for Scientific Development in Fenhe River Valley, Taiyuan Normal University, Taiyuan, Shanxi 030012, China;Research Center for Scientific Development in Fenhe River Valley, Taiyuan Normal University, Taiyuan, Shanxi 030012, China;Institute of Loess Plateau, Shanxi University, Taiyuan, Shanxi 030006, China;Institute of Loess Plateau, Shanxi University, Taiyuan, Shanxi 030006, China |
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| Abstract: | The spatio-temporal heterogeneity of soil moisture in Kelan County, Northwestern Shanxi Province was studied in wasteland, Caragana korshinskii forest land and Populus simonii forest land. The soil moisture was determined for the 0-600 cm profile in April, May, June and July. Results showed that:(1) Soil moisture changed between 3.34%~17.19% with irregular variation in the layer of 0-200 cm; However, as the soil depth increased from 200 to 600 cm, the soil moisture of wasteland was increasing, the soil moisture of Caragana korshinskii forest land was decreasing gently and the soil moisture of Populus simonii. forest land decreased at first and then increased gently, respectively.(2) The profile distribution of soil moisture had a significant difference(p<0.01) within different months and different land use types.(3) The variation coefficient of soil moisture was usually in the range of 0~30%, but some individual values are over 50%, suggesting that the structure of soil moisture presented overall stability except special points. |
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| Keywords: | soil moisture loess hilly region spatial heterogeneity ecological reconstruction |
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