[1]张健,刘国彬,许明祥,等.黄土丘陵区植被次生演替灌木初期土壤物理性质特征[J].水土保持研究,2008,15(04):101-104,109.
　ZHANG Jian,LIU Guo-bin,XU Ming-xiang,et al.Soil Physical Properties of Vegetation Secondary Succession on Early Shrub Stage in Loess Hill Gully[J].Research of Soil and Water Conservation,2008,15(04):101-104,109.
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黄土丘陵区植被次生演替灌木初期土壤物理性质特征

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 15 期数: 2008年04期 页码: 101-104,109 栏目: 出版日期: 2008-08-20
Title:
Soil Physical Properties of Vegetation Secondary Succession on Early Shrub Stage in Loess Hill Gully
作者:
张健1, 刘国彬1,2, 许明祥1,2, 李小利2, 周萍2
1. 西北农林科技大学, 陕西 杨陵 712100;
2. 中国科学院 水利部 水土保持研究所, 陕西 杨陵 712100
Author(s):
ZHANG Jian1, LIU Guo-bin1,2, XU Ming-xiang1,2, LI Xiao-li2, ZHOU Ping2
1. Northwest A & FUniversity, Yangling, shaanxi 712100, China;
2. Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, shaanxi 712100, China
关键词:
黄土丘陵区; 次生演替; 土壤物理性质; 灌木
Keywords:
loess hill gully; secondary succession; soil physical property; shrub
分类号:
S714.2
摘要:
研究了黄土丘陵区植被次生演替草灌过渡灌木初期的土壤物理性质特征。结果表明：当植被次生演替进展到草灌过渡灌木初期，除土壤含水量外，土壤容重、孔隙度、稳定入渗和水稳性团聚体都好于对照白羊草地，表明灌木树种定居的土壤物理条件一般要高于草本群落。植被演替的过程是植被与土壤相互作用复杂变化的过程，它们的相互反馈也是生态恢复的重要标志。随着植物群落的变化土壤也发生着不同程度变化。其中，土壤物理性质各个因子之间的变化是相互影响和相互联系的。土壤稳定入渗速率与土壤容重、土壤总孔隙度、土壤毛管孔隙度和土壤团聚体之间有显著的相关关系；土壤毛管孔隙度与土壤非毛管孔隙度线性显著负相关；土壤容重与土壤总孔隙度极显著负相关。
Abstract:
This paper studied the characteristics of soil physical properties during vegetation secondary succession from herb stage to shrub stage in loess hill gully.The results indicated that shrubs soil bulk density,porosity degree,soil infiltration and soil water stable aggregates was better than that of Bothriochloa ischaemun field.But soil water content is an exception.Soil physical properties of shrub tree were higher than that of herb community.The process of vegetation succession is an interaction and complicated changed process between vegetation and soil.Plant-soil interaction is the most important feedback in the processes of restoration and succession.Soil has different degree change with the change of plant communities.Thereinto,the change of different soil physical property factors is reciprocally influencing and relation.The soil infiltration rates has significant linear correlation with soil bulk density,total porosity,capillary porosity and soil water stable aggregate.Capillary porosity has negative linear correlation with non-capillary porosity (P<0.05).Soil bulk density has significant negative linear correlation with total porosity (P<0.01).

参考文献/References:

[1] 吴钦孝, 杨文治.黄土高原植被建设与可持续发展[M].北京:科学出版社, 1998.
[2] 梁一民, 李代琼, 从心海.吴旗沙打旺草地土壤水分及生产力特征[J].水土保持通报, 1990, 10(6):113-118.
[3] 王 力, 邵明安, 侯庆春.黄土高原土壤干层初步研究[J].西北农林科技大学学报:自然科学版, 2001, 29(4):34-38.
[4] 李裕元, 邵明安.子午岭植被自然恢复过程中植物多样性的变化[J].生态学报, 2004, 24(2):252-260.
[5] 邹厚远, 程积民, 等.黄土高原草原植被的自然恢复演替及调节[J].水土保持研究, 1998, 5(1):126-138.
[6] 王国梁, 刘国彬, 刘芳, 等.黄土沟壑区植被恢复过程中植物群落组成及结构变化[J].生态学报, 2003, 23(12):2550-2557.
[7] 杜 峰, 山 仑, 梁宗锁.陕北黄土丘陵区撂荒演替研究[J].草地学报, 2005, 13(4):328-333.
[8] 白文娟, 焦菊英, 马祥华, 等.黄土丘陵沟壑区退耕地自然恢复植物群落的分类与排序[J].西北植物学报, 2005, 25(7):1317-1322.
[9] 张成娥, 陈小利.黄土丘陵区不同撂荒年限自然恢复的退化草地土壤养分及酶活性特征[J].草地学报, 1997, 5(3):195-200.
[10] 温仲明, 焦峰, 刘宝元.黄土高原森林草原区退耕地植被自然恢复与土壤养分变化[J].应用生态学报, 2005, 16(11):2025-2029.
[11] 潘成忠, 上官周平, 刘国彬.黄土丘陵沟壑区退耕草地土壤质量演变[J].生态学报, 2006, 26(3):690-696.
[12] 巩 杰, 陈利顶, 傅伯杰, 等.黄土丘陵区小流域植被恢复的土壤养分效应研究[J].水土保持学报, 2005, 19(1):93-96.
[13] 侯扶江, 肖金玉, 南志标.黄土高原退耕地的生态恢复[J].应用生态学报, 2002, 13(8):923-929.
[14] 许明祥, 刘国彬.黄土丘陵区刺槐人工林土壤养分特征及演变[J].植物营养与肥料学报, 2004, 10(1):40-46.
[15] 杨小波, 张桃林, 吴庆书.海南琼北地区不同植被类型物种多样性与土壤肥力的[J].生态学报, 2002, 22(2):1990-1996.
[16] 中国科学院南京土壤研究所.土壤理化分析[M].上海:上海科学技术出版社, 1978.
[17] 杜峰, 山仑, 梁宗锁, 等.陕北黄土丘陵区撂荒演替过程中的土壤水分效应[J].自然资源学报, 2005, 20(5):669-678.
[18] 杨弘, 李忠, 等.长白山北坡阔叶红松林和暗针叶林的土壤水分物理性质[J].应用生态学报, 2007, 18(2):272-276.
[19] 张雅楠, 黄兴法, 毛丽丽, 等.土壤入渗性能自动测量系统原理与应用研究[J].农业工程学报, 2007, 23(4):99-104.
[20] 陈瑶, 张科利, 罗利芳, 等.黄土坡耕地弃耕后土壤入渗变化规律及影响因素[J].泥沙研究, 2005(5):45-50.
[21] 王国梁, 刘国彬, 周生路.黄土丘陵沟壑区小流域植被恢复对土壤稳定入渗的影响[J].自然资源学报, 2003, 18(5):529-535.
[22] 安树青, 王峥峰, 朱学雷, 等.土壤因子对次生森林群落演替的影响[J].生态学报, 1997, 17(1):45-50.
[23] 王政权, 王庆成.森林土壤物理性质的空间异质性研究[J].生态学报, 2000, 20(6):945-950.

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[9]程积民.宁南黄土丘陵区灌木林生产力的研究[J].水土保持研究,1996,3(01):129.
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[10]侯喜禄,白岗栓,曹清玉.黄土丘陵区湾塌地乔灌林土壤水分动态监测[J].水土保持研究,1996,3(02):57.
　Hou Xilu,Bai Gangshuan,Cao Qingyu.Dynamic Observation of Soil Moisture on Arbor and Shrubbery in Sinking Lands in Loess Hilly Region[J].Research of Soil and Water Conservation,1996,3(04):57.

备注/Memo

收稿日期:2007-12-27。
基金项目:国家自然科学基金重点项目 （90502007）；国家重点基础研究发展计划（2007CB407205）；中国科学院知识创新项目（KZCX2-XB2-05-03）
作者简介:张健（1980- ），男，吉林梨树人，在读硕士，主要从事植被恢复与环境效应方面的研究。E-mail：zhangjian12102@163.com
通讯作者:许明祥（1972- ），男，陕西吴旗人，副研究员，主要从事土壤侵蚀方面的研究。E-mail：xumx@nwsuaf.edu.cn

更新日期/Last Update: 1900-01-01