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喀斯特峰丛洼地土壤矿物质的组成特征与作用
  • ISSN号:1001-9332
  • 期刊名称:Chinese Journal of Applied Ecology
  • 时间:2012.3.3
  • 页码:685-693
  • 分类:S152.1[农业科学—土壤学;农业科学—农业基础科学]
  • 作者机构:[1]中国科学院亚热带农业生态研究所亚热带农业生态过程重点实验室,长沙410125, [2]江西农业大学,南昌330045, [3]中国科学院环江喀斯特农业生态试验站,广西环江547100
  • 相关基金:中国科学院西部行动计划项目(KZCX2-XB3-10)、中国科学院战略性先导科技专项(XDA05050205,XDA05070404)、中国科学院知识创新工程项目(KZCX-2-YW-436)、国家科技支撑计划项目(2010BAE00739)和国家自然科学基金项目(31070425,31000224,30970508,U1033004,31100329)资助.
  • 相关项目:喀斯特峰丛洼地森林生态系统的碳格局及驱动机制
中文摘要:

基于喀斯特峰丛洼地农作区、人工林、次生林、原生林4类典型生态系统动态监测样地(200 m×40 m)土壤矿质养分因子(7个)、植被(9个)、地形(4个)、土壤理化性状(10个)共计30个指标的全面调查取样分析,采用经典统计分析、主成分分析和典范相关分析探讨了土壤矿物质的组成特征、作用以及与植被、地形、其他土壤性状的耦合关系.结果表明:喀斯特峰丛洼地土壤矿物质组成以SiO2、Al2O3、K2O、Fe2O3为主,明显低于全球土壤平均背景值和同区域地带性红壤,CaO、MgO含量居中,MnO含量很低;不同生态系统土壤矿物质组成和变异不同,土壤的发育程度也不同,植被和土壤的原生性呈同比正相关,均有潜在的石漠化风险;4类生态系统景观异质性高,主成分分析的降维效果不好,土壤矿物质均为各生态系统的主要影响因子,且与植被、地形、其他土壤性状的关系非常密切,特别是SiO2、CaO和MnO,其中对植被的影响主要是物种多样性,对土壤则为有机质、全氮、全钾等主要养分.土壤矿物质是影响喀斯特峰丛洼地土壤肥力和植物生长发育的限制因子之一,有效利用矿物质资源、合理施用矿质养分对喀斯特退化生态系统的恢复与重建作用重大.

英文摘要:

Based on the investigation and analysis of seven soil mineral substance variables,nine vegetation factors,four topographical factors,and ten soil physicochemical factors in the 200 m×40 m dynamic monitoring plots in farmland,forest plantation,secondary forest,and primary forest in the depressions between hills in karst region,and by using traditional statistical analysis,principal component analysis(PCA),and canonical correlation analysis(CCA),this paper studied the compositional characteristics and roles of soil mineral substances as well as the coupling relationships between the mineral substances and the vegetation,topography,and other soil properties.In the depressions,soil mineral substances were mainly composed of SiO2,Al2O3,K2O,and Fe2O3,whose contents were obviously lower than the mean background values of the soils in the world and in the zonal red soils at the same latitudes.The soil CaO and MgO contents were at medium level,while the soil MnO content was very low.The composition of soil mineral substances and their variation degrees varied with the ecosystems,and the soil development degree also varied.There was a positive correlation between vegetation origin and soil origin,suggesting the potential risk of rock desertification.Due to the high landscape heterogeneity of the four ecosystems,PCA didn't show good effect in lowering dimension.In all of the four ecosystems,soil mineral substances were the main affecting factors,and had very close relationships with vegetation,topography,and other soil properties.Especially for SiO2,CaO,and MnO,they mainly affected the vegetation species diversity and the soil organic matter,total nitrogen,and total potassium.This study indicated that soil mineral substances were the one of the factors limiting the soil fertility and vegetation growth in the depressions between hills in karst region.To effectively use the soil mineral resources and rationally apply mineral nutrients would have significances in the restoration and reconstruction of karst degraded

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期刊信息
  • 《应用生态学报》
  • 北大核心期刊(2011版)
  • 主管单位:中国科学院
  • 主办单位:中国生态学学会 中国科学院沈阳应用生态研究所
  • 主编:沈善敏
  • 地址:沈阳市文化路72号
  • 邮编:110016
  • 邮箱:
  • 电话:024-83970393
  • 国际标准刊号:ISSN:1001-9332
  • 国内统一刊号:ISSN:21-1253/Q
  • 邮发代号:8-98
  • 获奖情况:
  • 中国自然科学核心期刊,中国科学院优秀期刊,中国期刊方阵“双效”期刊
  • 国内外数据库收录:
  • 俄罗斯文摘杂志,美国化学文摘(网络版),荷兰地学数据库,荷兰文摘与引文数据库,美国生物医学检索系统,美国生物科学数据库,英国动物学记录,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版)
  • 被引量:98742