[1]牛勇,汪滨,王玲,等.北京土石山区4种典型林分的水文效应研究[J].水土保持研究,2015,22(05):113-117,121.
　NIU Yong,WANG Bin,WANG Ling,et al.Study of Hydrological Functions of Four Types of Forest Stands in Rocky and Earthy Area of Beijing[J].Research of Soil and Water Conservation,2015,22(05):113-117,121.
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北京土石山区4种典型林分的水文效应研究

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 22 期数: 2015年05期 页码: 113-117,121 栏目: 出版日期: 2015-10-28
Title:
Study of Hydrological Functions of Four Types of Forest Stands in Rocky and Earthy Area of Beijing
作者:
牛勇1, 汪滨1, 王玲2, 蔡永茂2, 张志强1
1. 北京林业大学 水土保持学院 水土保持与荒漠化防治教育部重点实验室, 北京 100083;
2. 北京市八达岭林场, 北京 102112
Author(s):
NIU Yong1, WANG Bin1, WANG Ling2, CAI Yongmao2, ZHANG Zhiqiang1
1. Key Laboratory of Soil and Water Conservation and Desertification Combating, Ministry of Education, College of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China;
2. Beijing Badaling Forest Farm, Beijing 102112, China
关键词:
冠层截留; 枯落物; 水力学参数; 土石山区; 水文效应
Keywords:
canopy interception; forest litter; hydraulics parameter; rocky and earthy area; hydrological functions
分类号:
S715
摘要:
以北京土石山区4种典型林分的林冠层、枯落物层、土壤层3个水文作用层为研究对象，采用浸水法等传统测量方法，测定了不同林分的冠层截留量、树干径流量、穿透降雨量以及土壤和枯落物层的水力学参数，并分析了其水文效应。结果表明：不同林分的林冠截留能力相差较大，其中侧柏—黄栌混交林的冠层截留率最大为29.1%，其余依次为侧柏林、油松纯林和元宝枫纯林，油松纯林的树干径流量占降雨比例最大（5.8%），其余依次为侧柏—黄栌混交林、元宝枫纯林和侧柏林，各项林冠截留率与大多数在干旱半干旱地区取得结果较为一致。从月份尺度的变化趋势来看，不同林分的截留量均为6月最大，7月、8月、9月、10月和5月依次减小，即截留量与降雨量呈正比关系。4种林分枯落物总蓄积量范围为26.3～246.0 t/hm2，其中油松纯林的枯落物储量显著大于其他林分类型（p < 0.05），侧柏纯林、侧柏—黄栌混交林、元宝枫纯林依次次之，不同林分枯落物的最大持水量和有效持水量的大小排序与之一致。受土壤的物质构成、机械组成、根系的发育状况等因素影响，侧柏纯林的土壤孔隙度和饱和入渗速率（Ks）依次大于侧柏—黄栌混交林、油松纯林和元宝枫纯林。
Abstract:
Hydrological functions of three hydrological function layers of four forest types were investigated in forest stands of rocky and earthy area in Beijing. The traditional measurement methods were used to monitor throughfall, stemflow, interception loss, hydraulics parameters of forest litter and soil. The results indicated that the interception capacity of different vegetation was significantly different, with the maximal canopy interception of stand of mixed Platycladus orientalis (L.) Franco and Cotinus coggygria Scop. (29.1%), followed by stands of Platycladus orientalis (L.) Franco, Pinus tabuliformis, Acer truncatum. The stem flow ratio of stand Pinus tabuliformis was the highest (5.83%), which fitted the results obtained in arid and semi-arid region well. At the monthly scale, the maximal interception ratio appeared in June, followed July, August, October and May, and there was a positive correlation between interception and rainfall. The forest litter quantity of four stands ranged from 26.3 t/hm2 to 246.0 t/hm2, and the forest litter quantity of stand Pinus tabuliformis was much greater than the others (p < 0.05),followed by stands of mixed Platycladus orientalis (L.) Franco and Cotinus coggygria Scop., Platycladus orientalis (L.) Franco and Acer truncatum, as the same order of the maximum water holding capacity and available interception amount of forest litter. The soil porosity and Ks of stand of mixed Platycladus orientalis (L.) Franco and Cotinus coggygria Scop. were greater than the other stands with the influence of material composition, mechanical composition, root, etc.

参考文献/References:

[1] 赵海涛,程根伟,于新晓.山地森林生态系统水文循环与数学模拟[M].北京:科学出版社,2004.
[2] 王爱娟,章文波.林冠截留降雨研究综述[J].水土保持研究,2009,16(4):55-59.
[3] Rutter A J, Morton A J. A predictive model of rainfall interception in forests:Ⅲ. sensitivity of the model to stand parameters and meteorological variables[J]. The Journal of Applied Ecology,1977,14(2):567-588.
[4] Gash J H C. An analytical model of rainfall interception by forests[J]. Quarterly Journal of the Royal Meteorological Society,1979,105(443):43-55.
[5] Gash J H C, Lloyd C R, Lachaud G. Estimating sparse forest rainfall interception with an analytical model[J]. Journal of Hydrology,1995,170(1/4):79-86.
[6] 裴铁璠,刘家冈,韩绍文,等.树干径流模型[J].应用生态学报,1990,1(4):294-300.
[7] 叶吉,郝占庆,姜萍.长白山暗针叶林苔藓枯落物层的降雨截留过程[J].生态学报,2004,24(12):2859-2862.
[8] 刘兴明,刘贤德,车宗玺,等.祁连山青海云杉林区苔藓层对流域水文的影响[J].干旱区地理,2010,31(6):962-967.
[9] 朱兴武,张鸿昌,陈选,等.大通宝库林区森林枯枝落物层水文特征研究[J].青海农林科技,1993(4):1-6.
[10] 王金叶,田大伦,王彦辉,等.祁连山林草复合流域土壤水文效应[J].水土保持学报,2005(3):144-147.
[11] 吕刚,吴祥云,雷泽勇,等.辽西半干旱低山丘陵区人工林地表层土壤水文效应[J].水土保持学报,2008(5):204-208.
[12] 彭舜磊,陈昌东,刘沛松,等.豫西低山丘陵区不同植被恢复类型表层土壤入渗规律[J].湖北农业科学,2013,52(7):1549-1552.
[13] 黄茹,黄林,何丙辉,等.三峡库区不同林草治理措施下土壤入渗特征研究[J].西南大学学报:自然科学版,2013,35(9):119-126.
[14] 张焜,张洪江,程金花,等.重庆四面山三种人工林林冠截留效应研究[J].水土保持研究,2011,18(1):201-204.
[15] Teklehaimanot Z, Jarvis P G, Ledger D C. Rainfall interception and boundary layer conductance in relation to tree spacing[J]. Journal of Hydrology,1991,123(3/4):261-278.
[16] Viville D, Biron P, Granier A, et al. Interception in a mountainous declining spruce stand in the Strengbach catchment(Vosges, France)[J]. Journal of Hydrology,1993,144(1/4):273-282.
[17] 张志强.森林水文:过程与机理[M].北京:中国环境科学出版社, 2002.
[18] Putuhena W M, Cordery I. Estimation of interception capacity of the forest floor[J]. Journal of Hydrology,1996,180(1/4):283-299.
[19] Tietema A, Warmerdam B, Lenting E, et al. Abiotic factors regulating nitrogen transformations in the organic layer of acid forest soils:Moisture and pH[J]. Plant and Soil,1992,147(1):69-78.
[20] Dunne T. Field studies of hillslope flow processes[M]//Kirkby. Hillslopehydrolog. New York:John Wiley & Sons,1978.
[21] 何东宁,王占林,张洪勋.青海乐都地区森林涵养水源效能研究[J].植物生态学与地植物学学报,1991,15(1):71-78.
[22] 王贺年,余新晓,贾国栋,等.华北土石山区流域森林覆盖率对径流影响的定量分析[J].应用基础与工程科学学报,2013,21(3):432-441.
[23] 蔡永茂,许兰霞,张咏.八达岭林场的分类经营评价[J].北京林业大学学报,2003,25(S1):57-62.
[24] 姚永刚,王玲,张立,等.北京市八达岭风景区树木物候研究[J].林业实用技术,2006(1):7-9.
[25] 刘千,王平,熊伟,等.六盘山北侧叠叠沟小流域几种典型植被群落的水文功能研究[J].干旱地区农业研究,2013,31(4):193-199.
[26] 高开通,胡淑萍,刘鹏举,等.北京九龙山自然保护区典型林分枯落物水文效应研究[J].水土保持研究,2013(5):160-164.
[27] 王薇,孟杰,虎胆·吐马尔白. RETC推求土壤水动力学参数的室内试验研究[J].河北农业大学学报,2008,31(1):99-102.
[28] 黄承标,梁宏温.广西亚热带主要林型的树干茎流[J].植物资源与环境,1994,3(4):10-17.
[29] 陈波,孟成生,赵耀新,等.冀北山地不同海拔华北落叶松人工林枯落物和土壤水文效应[J].水土保持学报,2012,26(3):216-221.
[30] 赵忠,李鹏,王乃江.渭北黄土高原主要造林树种根系分布特征的研究[J].应用生态学报,2000,11(1):38-40.

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　QI Ji,SHI Yu,YU Xin-xiao,et al.Hydrological Function of Litters of the Main Tree Species in Beijing Mountainous Area[J].Research of Soil and Water Conservation,2011,18(05):73.

备注/Memo

收稿日期:2014-11-03;改回日期:2014-12-05。
基金项目:国家林业公益性行业科研专项“森林经营对生态系统碳水耦合变化的影响机理研究”（201204102）
作者简介:牛勇(1984-),男,山东-城县人,博士,研究方向为森林水文。E-mail:niuyong1988@qq.com
通讯作者:张志强(1967-),男,内蒙古呼和浩特人,博士,教授,主要从事森林水文研究。E-mail:zhqzhang@bjfu.edu.cn

更新日期/Last Update: 1900-01-01