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不同林分类型土壤水分物理性质及其海拔效应——以浙江省凤阳山为例
引用本文:田月亮,张金池,李海东,庄加尧,叶立新,刘胜龙.不同林分类型土壤水分物理性质及其海拔效应——以浙江省凤阳山为例[J].水土保持通报,2013,33(1):53-57,61.
作者姓名:田月亮  张金池  李海东  庄加尧  叶立新  刘胜龙
作者单位:1. 南京林业大学森林资源与环境学院,江苏南京,210037
2. 环境保护部南京环境科学研究所,江苏南京,210042
3. 凤阳山自然保护区,浙江龙泉,323700
基金项目:国家公益性行业科研专项“典型森林植被对水资源形成过程的调控研究”(201104005)
摘    要:以浙江省凤阳山常绿阔叶林和针阔混交林为例,通过野外调查和室内测定土壤容重、土壤孔隙度及土壤含水量等,研究了中亚热带主要林分类型的土壤水分物理性质及其海拔影响.结果表明,在0-60 cm土层中,随着深度的增加土壤容重逐渐增大,土壤总孔隙度、毛管孔隙度、最大持水量、毛管持水量、最小持水量逐渐减小.在海拔300~I 355 m高程范围随着海拔升高土壤容重平均值逐渐减小,土壤总孔隙度、毛管孔隙度、最大持水量、毛管持水量、最小持水量、土壤贮水量平均值均增大;土壤排水能力平均值为:海拔900 m>海拔600 m>海拔1 355 m>海拔300 m.同一海拔4种林分类型土壤容重平均值:人工杉木林>针阔混交林>人工柳杉林>常绿阔叶混交林;土壤总孔隙度、土壤最大持水量、毛管持水量、最小持水量、土壤贮水量平均值均表现为人工柳杉林优于其他3种林分类型;土壤排水能力平均值表现为:常绿阔叶混交林>人工杉木林>人工柳杉林>针阔混交林.综合分析,同一海拔常绿阔叶林水源涵养及保持水土能力要高于人工柳杉林.

关 键 词:土壤持水量  孔隙度  容重  海拔高度  林分类型
收稿时间:1/8/2012 12:00:00 AM
修稿时间:2012/3/24 0:00:00

Physical Characteristics of Soil Moisture and Their Altitude Effects for Different Forest Stand Types in Fengyang Mountains of Zhejiang Province
TIAN Yue-liang,ZHANG Jin-chi,LI Hai-dong,ZHUAN Jia-yao,YE Li-xin and LIU Sheng-long.Physical Characteristics of Soil Moisture and Their Altitude Effects for Different Forest Stand Types in Fengyang Mountains of Zhejiang Province[J].Bulletin of Soil and Water Conservation,2013,33(1):53-57,61.
Authors:TIAN Yue-liang  ZHANG Jin-chi  LI Hai-dong  ZHUAN Jia-yao  YE Li-xin and LIU Sheng-long
Institution:1.College of Forest Resources and Environment,Nanjing Forestry University,Nanjing,Jiangsu 210037,China;2.Nanjing Institute of Environmental Science,Ministry of Environmental Protection, Nanjing,Jiangsu 210042,China;3.Fengyang Mountain Natural Reserve,Longquan,Zhejiang 323700,China)
Abstract:By taking evergreen and deciduous broad-leaved mixed forests in the Fengyang Mountains of Zhejiang Province for an instance,the physical characteristics of soil moisture and its effects for the main different forest stand types in the mid subtropical zone are studied through field survey and laboratory measurements for soil bulk density,soil porosity and soil moisture content.Between 0and 60cm soil layer,soil bulkdensity rises gradually and total soil pore space,capillary porosity,maximum holding capacity,capillarywater capacity and minimum water holding capacity decrease gradually,as soil depth increases.Between 300and 1 355maltitude rank,the averaged value of soil bulk density decreases gradually and the averaged valuesof total soil pore space,capillary porosity,maximum holding capacity,capillary water capacity,the averagewater holding capacity and soil water capacity increase,respectively,as the altitude increase.The averagedvalues of soil drainage ability for the four forest stand types rank in the order of 900maltitude>600maltitude>1 355maltitude>300maltitude.The averaged values of soil bulk density for the four forest standtypes at the same altitude rank in the order of Chinese fir plantation>coniferous broad-leaved mixed forest>Cryptomeria fortunei plantation>evergreen broad-leaved mixed forest.Cryptomeria fortunei plantation is superior to the other three forest stand types in the averaged values of the total soil pore space,the maximum soil water holding capacity,capillary water capacity,the minimum water holding capacity andwater capacity.The averaged values of soil drainage ability rank in the order of evergreen broad-leaved mixedforest> Chinese fir plantation>Cryptomeria fortunei plantation>coniferous broad-leaved mixed forest.In summary,the water conservation and soil water conservation abilities of evergreen broad-leaved mixedforest are higher than those of Cryptomeria fortunei plantation at the same altitude.
Keywords:soil water holding capacity  porosity  bulk density  altitude  forest stand type
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