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内蒙半干旱低山区不同纯林土壤腐殖质分异特征及其与其他生物化学性质的关系
引用本文:张晓曦,刘增文,邴塬皓,朱博超,黄良嘉.内蒙半干旱低山区不同纯林土壤腐殖质分异特征及其与其他生物化学性质的关系[J].生态学杂志,2014,25(10):2819-2825.
作者姓名:张晓曦  刘增文  邴塬皓  朱博超  黄良嘉
作者单位:(;1.西北农林科技大学水土保持研究所, 陕西杨凌 712100; ;2.西北农林科技大学资源环境学院, 陕西杨凌 712100; ;3.农业部西北植物营养与农业环境重点实验室, 陕西杨凌 712100; ;4.西北农林科技大学林学院, 陕西杨凌 712100)
摘    要:纯林土壤腐殖质含量及其构成是否会因枯落叶组成的单一性和单优群落环境的特殊性而发生分异变化是关系到森林可持续经营的关键问题.本文以内蒙半干旱低山区的6种典型纯林为研究对象,研究了不同树种纯林土壤腐殖质分异特征及其与其他生物化学性质的关系.结果表明:云杉和白桦林地土壤的腐殖质含量、缩合程度和稳定性均较高,其次为小叶杨和落叶松林地,再次为白榆林地,而油松林地土壤的腐殖质含量和缩合程度均最低、稳定性最差.土壤微生物生物量和磷酸酶活性与腐殖质各组分的积累及其稳定性存在相互促进作用;过氧化氢酶和脱氢酶活性则与土壤腐殖质存在相互抑制作用,且脱氢酶活性的提高可能破坏腐殖质的稳定性.速效N含量与腐殖质积累及其稳定性呈正相关,而全量Cu、Fe、Zn含量与腐殖质呈负相关,全Cu、Fe的增加可能会破坏腐殖质的稳定性.纯林环境及其枯落叶性质的特殊性是造成腐殖质分异的重要原因,混交改造或增加林下植被是改善土壤腐殖质构成的根本措施.

关 键 词:纯林土壤  腐殖质  生物化学性质  枯落叶

Soil humus differentiation and correlation with other soil biochemical properties in pure forests in semi arid low hilly area of Inner Mongolia,China.
ZHANG Xiao-xi,LIU Zeng-wen,BING Yuan-hao,ZHU Bo-chao,HUANG Liang-jia.Soil humus differentiation and correlation with other soil biochemical properties in pure forests in semi arid low hilly area of Inner Mongolia,China.[J].Chinese Journal of Ecology,2014,25(10):2819-2825.
Authors:ZHANG Xiao-xi  LIU Zeng-wen  BING Yuan-hao  ZHU Bo-chao  HUANG Liang-jia
Institution:(;1.Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, Shaanxi, China; ;2.College of Natural Resources and Environment, Northwest A&F University, Yangling 712100, Shaanxi, China;;Ministry of Agriculture Key Laboratory of Plant Nutrition and the Agri environment in Northwest China, Yangling 712100, Shaanxi, China; ;College of Forestry, Northwest A&F University, Yangling 712100, Shaanxi, China
Abstract:Whether the content and composition of soil humus in pure forest change due to its simple component of litter and specificity of single species dominant community is a key problem for forest sustainable management. In this study, soils from 6 kind of pure forests in semi arid low hilly area of Inner Mongolia were collected and their humus and other biochemical properties were mea sured to investigate the differentiation of soil humus and the impact factors. The results showed that the soil of Picea asperata and Betula platyphylla pure forests had the highest contents of humus and better condensation degrees and stabilities, followed by that of Populus simonii, Larix principis rupprechtii and Ulmus pumila pure forests, while the soil of Pinus tabuliformis pure forest had the lowest content of humus, condensation degree and stability. There were significant positive correlations between soil microorganism biomass, activity of phosphatase and the content and stability of soil humus. In contrast, the soil peroxidate, dehydrogenase activity and soil humus content showed significant negative correlations with each other. Furthermore, the enhancement of dehydrogenase activity might decrease the stability of humus. There were significant positive correlations between available N and the content and stability of soil humus, but total Cu, Zn and Fe had negative correlations with them, and total Cu and Fe might reduce the stability of humus as well. The particularity of pure forest environment and litter properties might be the key inducement to soil humus differentiation, thus reforming the pure forest through mixing with other tree species or planting understory vegetation would be the fundamental way to improve the soil humus composition and stability.
Keywords:soil of pure forest  humus  biochemical property  litter  
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