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[1]YANG Liangchen,ZHANG Nan.Water Conservation Capacity of Litter and Soil Layer in Three Mixed Forests in Along the Dam Area[J].Research of Soil and Water Conservation,2019,26(03):253-258.

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Water Conservation Capacity of Litter and Soil Layer in Three Mixed Forests in Along the Dam Area

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 26 Number of periods: 2019 03 Page number: 253-258 Column: Public date: 2019-04-12

Title:: Water Conservation Capacity of Litter and Soil Layer in Three Mixed Forests in Along the Dam Area

Author(s):: YANG Liangchen¹, ZHANG Nan²; 1. Shexian Vocational and Technical Education Center of Hebei Province, Shexian, Hebei 056400, China;
2. Mulan-Weichang Forestry Administration of Hebei Province, Weichang, Hebei 068450, China

Keywords:: along the dam area; litter layer; soil layer; water conservation

CLC:: S715.3

DOI:: -

Abstract:: In order to study the water conservation capacity of the litter layer and soil layer of three mixed forest types along the dam area, the indoor immersion method and the double ring knife method were used to examine the water conservation capacity of the litter layer and soil layer of three mixed forests. The results showed that:(1) the biomass of litter decreased in the order coniferous and broad-leaved mixed forest > broad-leaved mixed forest > coniferous mixed forest; (2) the maximum water holding capacity decreased in the sequence broad-leaved mixed forest > coniferous and broad-leaved mixed forest > coniferous mixed forest; effective storage decreased in the order broad-leaved mixed forest > coniferous and broad-leaved mixed forest > coniferous mixed forest; water holding capacity and water immersion time; the regression equation was expressed as Q=alnt+b(R²>0.89), and the regression equation of water holding rate and water immersion time was described as V=Ktⁿ (R²>0.99); (3) the soil total porosity, non-capillary porosity and capillary porosity were higher in the broad-leaved mixed forest than the other two mixed forests, indicating that the geographical environment of broad-leaved mixed forest was more conducive to forest growth and water conservation; non-capillary porosity was closely related to soil water holding capacity, and its size was the same as soil water holding capacity, which decreased in the order broad-leaved mixed forest > coniferous and broad-leaved mixed forest > coniferous mixed forest, and the differences of initial infiltration rates of three forest layers were relatively large, and the initial infiltration rates decreased in the order coniferous mixed forest>broad-leaved mixed forest>coniferous and broad-leaved mixed forest; The regression equation of infiltration rate and infiltration time was described as f=at^-b (R²>0.94).

References:: [1] 徐娟,余新晓,席彩云.北京十三陵不同林分枯落物层和土壤层水文效应研究[J].水土保持学报,2009,23(3):189-193.
[2] 姜海燕,赵雨森,陈祥伟,等.大兴安岭岭南几种主要森林类型土壤水文功能研究[J].水土保持学报,2007,21(3):149-153.
[3] 张晓蓓.宁夏六盘山南侧华北落叶松人工林生态水文影响的密度效应评价[D].河北保定:河北农业大学,2012.
[4] 张宁,梁丽双,常月梅,等.冀北山地落叶松4种典型林分的结构研究[J].中南林业科技大学学报,2015,22(6):20-27.
[5] 张宁,郭宾良,于士涛,等.冀北山地4种典型落叶松林分生态功能研究[J].水土保持研究,2015,22(2):320-327.
[6] 孙艳红,张洪江,杜士才,等.四面山不同林地类型土壤特性及其水源涵养功能[J].水土保持学报,2009,23(5):109-113.
[7] 赵阳,余新晓,吴海龙,等.华北土石山区典型森林枯落物层和土壤层水文效应[J].水土保持学报,2011,25(6):148-152.
[8] 白晋华,胡振华,郭晋平.华北山地次生林典型森林类型枯落物及土壤水文效应研究[J].水土保持学报,2009,23(2):84-89.
[9] 梁晓娇,王树力.阿什河源头不同类型红松人工林枯落物与其土壤水文特性[J].水土保持学报,2017,31(1):140-145.
[10] 杨振奇,秦富仓,李晓琴,等.砒砂岩区主要造林树种枯落物及林下土壤持水特性[J].水土保持学报,2017,31(3):118-122.
[11] 谈正鑫,万福绪,张涛.盱眙人工林枯落物及土壤水文效应研究[J].水土保持研究,2015,22(4):184-188.
[12] 张焜.重庆四面山4种类型天然林水文功能研究[D].北京:北京林业大学,2012.

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