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土地利用变化对海南土壤水源涵养功能的影响
引用本文:文志,赵赫,刘磊,欧阳志云,郑华,米红旭,李彦旻.土地利用变化对海南土壤水源涵养功能的影响[J].生态学杂志,2017,28(12):4025-4033.
作者姓名:文志  赵赫  刘磊  欧阳志云  郑华  米红旭  李彦旻
作者单位:1.中国科学院生态环境研究中心城市与区域生态国家重点实验室, 北京 100085 ;2.中国科学院大学, 北京 100049 ;3.海南鹦哥岭国家级自然保护区管理站, 海南白沙 572800 ;4.中国科学院城市环境与健康重点实验室/中国科学院城市环境研究所, 福建厦门 361021 ;5.厦门城市代谢重点实验室, 福建厦门 361021
基金项目:本文由国家重点研发计划项目(2016YFC0503401)资助
摘    要:热带地区已有大量原始林转变为其他土地利用类型,影响了陆地生态系统的水源涵养功能.为了明确热带原始林转变为其他土地类型对土壤水源涵养功能的影响,在海南中部山区选择4种典型土地利用类型,包括林龄大于100年的原始林(VF)、10年生次生林(SF)、12年生槟榔林(AF)和35年生橡胶林(RF),评估土地利用变化对土壤持水性能和水源涵养功能指数(SWI)的影响.结果表明: 与原始林相比,表层土壤(0~10 cm)中,其他土地类型土壤持水性能指标均降低,12年槟榔林各土层指标均最低.土壤含水量和最大持水量与植被郁闭度、土壤有机质和土壤容重显著相关,表明郁闭度、土壤有机质和紧实度的改变是土壤持水性能变化的重要原因.与原始林相比,次生林、槟榔林和橡胶林土壤水源涵养功能分别减少27.7%、54.3%和11.5%,不同土层的差异各异,橡胶林仅表层土壤水源涵养功能显著降低.植被郁闭度、土壤有机质和土壤容重可解释土壤水源涵养功能变量的83.3%.土地利用转变显著改变了土壤持水性能和土壤水源涵养功能,相比12年槟榔林,35年橡胶林能更好地保持土壤水分,土地管理中增加土壤有机质和减少土壤紧实度可改善土壤持水性能及水源涵养功能.

关 键 词:土地利用变化  土壤持水性能  土壤水源涵养  海南
收稿时间:2017-05-22

Effects of land use changes on soil water conservation in Hainan Island,China
WEN Zhi,ZHAO He,LIU Lei,OUYANG Zhi-yun,ZHENG Hua,MI Hong-xu,LI Yan-min.Effects of land use changes on soil water conservation in Hainan Island,China[J].Chinese Journal of Ecology,2017,28(12):4025-4033.
Authors:WEN Zhi  ZHAO He  LIU Lei  OUYANG Zhi-yun  ZHENG Hua  MI Hong-xu  LI Yan-min
Abstract:In tropical areas, a large number of natural forests have been transformed into other plantations, which affected the water conservation function of terrestrial ecosystems. In order to clari-fy the effects of land use changes on soil water conservation function, we selected four typical land use types in the central mountainous region of Hainan Island, i.e., natural forests with stand age greater than 100 years (VF), secondary forests with stand age of 10 years (SF), areca plantations with stand age of 12 years (AF) and rubber plantations with stand age of 35 years (RF). The effects of land use change on soil water holding capacity and water conservation (presented by soil water index, SWI) were assessed. The results showed that, compared with VF, the soil water holding capacity index of other land types decreased in the top soil layer (0-10 cm). AF had the lowest soil water holding capacity in all soil layers. Soil water content and maximum water holding capacity were significantly related to canopy density, soil organic matter and soil bulk density, which indicated that canopy density, soil organic matter and compactness were important factors influencing soil water holding capacity. Compared to VF, soil water conservation of SF, AF and RF were reduced by 27.7%, 54.3% and 11.5%, respectively. The change of soil water conservation was inconsistent in different soil layers. Vegetation canopy density, soil organic matter and soil bulk density explained 83.3% of the variance of soil water conservation. It was suggested that land use conversion had significantly altered soil water holding capacity and water conservation function. RF could keep the soil water better than AF in the research area. Increasing soil organic matter and reducing soil compaction would be helpful to improve soil water holding capacity and water conservation function in land management.
Keywords:land use change  soil water holding capacity  soil water conservation  Hainan Island
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