PDF Download

[1]SI Bin,YAO Xiao-hua,REN Hua-dong,et al.Study on Soil Physical and Chemical Properties in the Process of Vegetation Succession in Karst Area of Eastern Yunnan[J].Research of Soil and Water Conservation,2009,16(01):145-148.

Copy

Study on Soil Physical and Chemical Properties in the Process of Vegetation Succession in Karst Area of Eastern Yunnan

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 16 Number of periods: 2009 01 Page number: 145-148 Column: Public date: 2009-02-20

Title:: Study on Soil Physical and Chemical Properties in the Process of Vegetation Succession in Karst Area of Eastern Yunnan

Author(s):: SI Bin^1,2,3, YAO Xiao-hua¹, REN Hua-dong¹, LI Sheng¹, HE Bing-hui²; 1. Research Institute of Subtropical Forestry, CAF, Fuyang, Zhejiang 311400, China;
2. School of Resources and Environment, Southwest University, Beibei, Chongqing 400716, China;
3. The Committee of Shuicheng Country C.C.P, Shuicheng, Guizhou 553600, China

Keywords:: karst vegetation; rocky desertification; restoring of vegetation; nutritions of soil; eastern of Yunnan

CLC:: S158.1;X171.4

DOI:: -

Abstract:: The process of natural succession of restoring vegetation in eastern Yuannan after rocky desertification in Karst area appearing was divided into the herbosa stage, the stage of herbosa-shrub, the shrub stage, the stage of subaltern tree forest, the stage of Lithocarpus dealbatus-Quercus aquifolioies forest, the stage of Sawtooth oak-Quercus aquifolioies forest and the stage of Quercus aquifolioies forest. The physical and chemical properties of soil were studied by using space insteading of time. The results showed that, in the process of vegetation succession in Karst area in eastern Yunnan, the bulk density of soil decreased gradually from the stage of herbosa-shrub, and the least value appeared in the stage of Sawtooth oak-Quercus aquifolioies forest, then the bulk density of soil rose in the stage of Quercus aquifolioies forest. But the soil porosity was contrary to the bulk density of soil. The soil was weak acid in the whole proless of succession. The content of OM, virtual nutritions and total N rose from the stage of herbosa-shrub and reached the most value in the stage of Quercus aquifolioies forest. The content of total P rose firstly, then decreased, rosed finally and the two peaks of wave appeared in the stage of Lithocarpus dealbatus-Quercus aquifolioies forest and the stage of Quercus aquifolioies forest. The content of total K rosed gradually and reached the most in the stage of Lithocarpus dealbatus-Quercus aquifolioies forest, then decreased.

References:: [1] 王世杰.喀斯特石漠化概念演绎及其科学内涵的探讨[J].中国岩溶, 2002, 21(2):101-105.
[2] 李阳兵, 王世杰, 容丽.关于喀斯特石漠和石漠化概念的讨论[J ].中国沙漠, 2004, 24(6):689-695.
[3] 王德炉, 朱守谦, 黄宝龙.石漠化的概念及其内涵[J].南京林业大学学报:自然科学版, 2004, 28(6):87-90.
[4] 俞遵典.论喀斯特地貌的成因与演化[J].云南地质, 2003, 22(1):1-15.
[5] 李阳兵.西南岩溶山地生态环境研究进展与若干问题[J].云南地理环境研究, 2006, 18(2):61-65.
[6] 蔡秋, 陈梅琳.贵州喀斯特山区环境特征与生态系统的恢复和重建[J].农业系统科学与综合研究, 2001, 17(1):49-53.
[7] 苏维词.贵州喀斯特山区生态环境脆弱性及其生态整治[J].中国环境科学, 2000, 20(6):547-551.
[8] 苏维词, 杨华, 李晴, 等.我国西南喀斯特山区土地石漠化成因及防治[J].土壤通报, 2006, 37(3):447-451.
[9] 司彬, 何丙辉, 姚小华, 等.喀斯特石漠化形成原因及植被恢复途径探讨[J].江西农业大学学报, 2006, 28(3):392-396.
[10] 龙健, 江新荣, 邓启琼, 等.贵州喀斯特地区土壤石漠化的本质特征研究[J].土壤学报, 2005, 42(3):419-427.
[11] 涂成龙, 林昌虎, 何腾兵, 等.黔中石漠化地区生态恢复过程中土壤养分变异特征[J].水土保持通报, 2004, 24(6):22-25.
[12] 罗海波, 宋光煜, 何腾兵, 等.贵州喀斯特山区石漠化治理过程中土壤质量特性研究[J].水土保持学报, 2004, 18(6):112-115.
[13] 刘方, 王世杰, 刘元生, 等.喀斯特石漠化过程土壤质量变化及生态环境影响评价[J].生态学报, 2005, 25(3):639-644.
[14] 朱海燕, 刘忠德, 钟章成.喀斯特退化生态系统不同恢复阶段土壤质量研究[J].林业科学研究, 2006, 19(2):248-252.
[15] 龙健, 李娟, 黄昌勇.我国西南地区的喀斯特环境与土壤退化及其恢复[J].水土保持学报, 2002, 16(5):5-8.
[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.

Similar References:

Memo

Last Update: 1900-01-01