四川卧龙岷江冷杉林小流域土壤水分的时空分布特征及变异性Spatiotemporal Distribution Characteristics and Variability Coefficient of Soil Moisture in a Small Abies faxoniana Forest Catchment in Wolong,Sichuan Province
张瑞蒲,吕瑜良,刘兴良
ZHANG Rui-pu 1 L Yu-liang2 LIU Xing-liang3(1.Kunyushan Forest Farm of Yantai City,Yantai 264000,China
摘要(Abstract):
本文应用CNC503DR型中子土壤水分仪,在四川卧龙亚高山暗针叶林生态系统定位站,研究了林分和小流域尺度上岷江冷杉林土壤水分的时空分布特征及变异性。结果表明:研究期间,小流域土壤平均容积含水量在0.59~0.66之间,不同群落类型之间,差异比较明显,且随时间的变化规律不同;小流域内土壤剖面的平均容积含水量在0.52~0.77之间,平均值为0.60,土壤表层最高,45 cm深度最低;随着海拔升高,土壤含水量增加,但超过3 700 m则减少;不同坡向,土壤含水量在0~30 cm土层半阴坡高于半阳坡,30 cm以下土层则相反;不同坡位,土壤含水量下坡最高,其次是中坡,上坡最低;小流域土壤水分变异系数在0.217 6~0.409 8之间,不同群落类型之间差异显著,随着土层剖面深度增加而减小,随着海拔升高而减小,半阴坡高于半阳坡,下坡大于中坡和上坡。
In this paper,based on field data collected by a CNC503DR soil moisture neutron probe device in sub-alpine dark coniferous forest ecosystem station during the period from July to October,researches were conducted on quantified spatial and temporal distribution characteristics and variability coefficient of soil moisture in Abies faxoniana forest at both stand scale and catchment scale.The results showed that the mean volumetric soil moisture content in the catchment varied from 0.59 to 0.66 from July to October,which had slightly differences among different communities.The highest soil moisture content occurred in the subsurface soil layer while the lowest soil moisture content was found in below 45 cm soil depth.With the ascending of altitude,an increasing trend was firstly found in soil moisture content(SMC),however,when altitude exceeded 3 700 m,SMC showed an decreasing trend.Compared with the southwest-aspect slope,the northeast-aspect slope showed higher SMC in 0~30 cm soil depth while lower SMC appeared in soil depth below 30 cm.The soil moisture of the lower slopes was higher than that of the upper slopes.The coefficient of variability(CV) of soil moisture at catchment scale was 0.22~0.41.The CV increased with increasing SMC while decreased with increasing soil depth.The CV at northeast-aspect was higher than that at southwest-aspect,at lower slope higher than that at middle slope and upper slope.
关键词(KeyWords):
亚高山;暗针叶林;植被;岷江冷杉;土壤水分
Sub-alpine,Dark coniferous forest,Vegetation,Abies faxoniana,Soil moisture
基金项目(Foundation): 国家重点基础研究发展规划项目(G2002CB111504);; 西南大学博士基金(SWUB2008009)
作者(Author):
张瑞蒲,吕瑜良,刘兴良
ZHANG Rui-pu 1 L Yu-liang2 LIU Xing-liang3(1.Kunyushan Forest Farm of Yantai City,Yantai 264000,China
DOI: 10.16779/j.cnki.1003-5508.2010.06.002
参考文献(References):
- [1]Chang Z H,Lu Z H,Guan WB.Water holding effect of subalpinedark coniferous forest soil in Gongga Mountain,China.Journal ofForestry Research,2003,14(3):205~209.
- [2]Famiglietti J S,Rudnicki J W,Rodell M.Variability in surfacemoisture content along a hillslope transect:Rattlesnake Hill,Tex-as.Journal of Hydrology,1998,210:259~281.
- [3]Gimona A,Birnie R V.Spatio-temporal modelling of broad scaleheterogeneity in soil moisture content:a basis for an ecologicallymeaningful classification of soil landscapes.Landscape Ecology,2002,17:27~41
- [4]Iverson L R,Dale M E,Scott C T,et al.GIS-derived integratedmoisture index to predict forest composition and productivity of O-hio forests USA.Landscape Ecology,1997,12:331~348.
- [5]Neave HM,Cunningham R B,Norton TW,et al.Biological inven-tory for conservation evaluation 3.Relationships between birds,vegetation and environmental attributs in souther Austrilia.ForestEcology and Management,1998,85:197~218.
- [6]Rodrigo A,Recous S,Neil C,et al.Modelling temperature andmoisture effects on C-N transformations in soils:comparions ofnine models.Ecological Modelling,1997,102:325~339
- [7]Teuling AJ,Troch P A.Simulating soil moisture variability dynam-ics,in Proceedings of the 2nd international CAHMDA workshopon:The Terrestrial Water Cycle:Modelling and Data AssimilationAcross Catchment Scales,edited by A.J.Teuling,H.Leijnse,P.A.Troch,J.Sheffield and E.F.Wood,pp.81~85,Prince-ton,NJ,2004,October:25~27.
- [8]Wei M Y.Soil moisture:Report of a workshop held in Tiburon,California,25-27 January 1994.NASAConference Publication,1995,3319:80.
- [9]Wu W,Dickinson R E.Time Scales of Layered Soil Moisture Mem-ory in the Context of Land-Atmosphere Interaction.Journal of Cli-mate,2004,17:2752~2764
- [10]Xiong S,Johansson ME,Hughes F M R,et al.Interactive effectsof soil moisture,vegetation canopy,plant,litter and seed additionon plant diversity in a wetland community.Ecology,2003,91:976~986.
- [12]陈东立,余新晓,廖邦洪.中国森林生态系统水源涵养功能分析[J].世界林业研究,2005,18(1):49~54.
- [13]程金花,张洪江,余新晓,等.贡嘎山冷杉纯林地被物及土壤持水特性[J].北京林业大学学报,2002,24(3):45~49.
- [14]高甲荣,尹婧,牛健植,等.长江上游亚高山暗针叶林林地水文作用初探[J].北京林业大学学报,2002,24(4):75~79.
- [15]李崇巍岷江上游生态系统空间格局与生态水文过程模拟[D].北京师范大学博士学位论文,2005.
- [16]刘世荣,孙鹏森,王金锡,等.长江上游森林植被水文功能研究[J].自然资源学报,2001,16(5):451-456
- [17]刘世荣,温远光,王兵,等.中国森林生态系统水文生态规律[M].北京:中国林业出版社,1996
- [18]吕瑜良,刘世荣,孙鹏森,等.川西亚高山暗针叶林叶面积指数的季节动态与空间变异特征[J].林业科学,2007,43(8):1~7
- [19]马雪华.森林水文学[M].北京:中国林业出版社,1993.
- [20]马雪华.四川米亚罗地区高山冷杉林水文作用的研究[J].林业科学,1987,23(3):253~265.
- [21]王军,傅伯杰,蒋小平.土壤水分异质性的研究综述[J].水土保持研究,2002,9(1):1~5.
- [22]余新晓,赵玉涛,张志强,等.长江上游亚高山暗针叶林土壤水分入渗特征研究[J].应用生态学报,2003,14(1):15~19.
- [24]张保华,何毓蓉,周红艺,等.长江上游亚高山针叶林土壤水分入渗性能及.影响因子[J].四川林业科技,2003,24(1):61~64.
- [25]张保华,何毓蓉,周红艺,等.贡嘎山东坡亚高山森林土壤水分动态变化分析[J].西南农业学报,2003,16(增刊):98~100.
- [26]张远东,赵常明,刘世荣.川西亚高山人工云杉林和自然恢复演替系列的林地水文效应[J].自然资源学报,2004,19(6):761~768.
- [27]张志强.森林水文:过程与机制[M].北京:中国环境科学出版社,2003.