荒漠灌丛降雨再分配对土壤pH值的影响

官方微信

CN 62-1070/P
ISSN 1000-694X
双月刊创刊于1981年

高级检索

作者投稿专家审稿编辑办公

2013 , Vol. 33 >Issue 5: 1400 - 1405

DOI: https://doi.org/10.7522/j.issn.1000-694X.2013.00205

生物与土壤

荒漠灌丛降雨再分配对土壤pH值的影响

张亚峰1 ,
2 ,
王新平1 ,
虎瑞1 ,
2 ,
潘颜霞1

展开

1.中国科学院寒区旱区环境与工程研究所沙坡头沙漠试验研究站, 甘肃兰州 730000;
2.中国科学院大学, 北京 100049

收稿日期: 2012-08-17

修回日期: 2012-08-28

网络出版日期: 2012-08-28

收起

Effects of Rainfall Redistribution Induced by Xerophytic Vegetation on Soil pH

ZHANG Ya-feng1 ,
2 ,
WANG Xin-ping1 ,
HU Rui1 ,
2 ,
PAN Yan-xia1

Expand

1.Shapotou Desert Research and Experiment Station, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;
2.University of Chinese Academy of Sciences, Beijing 100049, China

Received date: 2012-08-17

Revised date: 2012-08-28

Online published: 2012-08-28

Fold

摘要

对腾格里沙漠东南缘沙坡头地区1989年建植人工植被区优势固沙灌木柠条（Caragana korshinskii）和半灌木油蒿（Artemisia ordosica）树干茎流及穿透雨的pH值,以及灌丛基部、灌丛下和灌丛外裸地0～10 cm和10～20 cm剖面深度土壤pH值分别进行测定,并与大气降雨pH值进行比较,以探讨荒漠灌丛降雨再分配对土壤pH值空间变异的影响。结果表明:大气降雨pH值最高,穿透雨pH值次之,树干茎流pH值最低,三者之间具有显著差异（p<0.05）。灌丛外裸地土壤pH值最高,灌丛下次之,树干基部最低。总体而言,0～10 cm剖面深度土壤pH值小于其下方10～20 cm剖面深度土壤pH值。柠条灌丛产生的树干茎流对土壤的酸化作用强于油蒿灌丛。树干茎流和穿透雨的酸化作用是导致土壤pH值从灌丛间裸地到灌丛基部方向上降低的一个重要原因。

关键词： 树干茎流; 穿透雨; 大气降雨; pH值; 土壤; 柠条（Caragana korshinskii）; 油蒿（Artemisia ordosica）

本文引用格式

张亚峰1 , 2 , 王新平1 , 虎瑞1 , 2 , 潘颜霞1 . 荒漠灌丛降雨再分配对土壤pH值的影响[J]. 中国沙漠, 2013 , 33(5) : 1400 -1405 . DOI: 10.7522/j.issn.1000-694X.2013.00205

Abstract

We measured the pH of gross rainfall, stemflow and throughfall, and the pH of soils that are adjacent to the shrub base, beneath the canopy and in the intershrub spaces of two dominant desert shrubs (Caragana korshinskii and Artemisia ordosica), respectively, in the revegetation area established in 1989 of Shapotou area, at the southeastern edge of the Tengger Desert. The study aimed to examine the effects of rainfall redistribution induced by xerophytic vegetation on soil pH variations. Significant differences (p<0.05) in pH were found between stemflow, throughfall and gross rainfall, with the highest in the gross rainfall, followed by throughfall and stemflow. Soil pH in the intershrub spaces was the highest, followed by that beneath shrub canopy and that adjacent to the shrub base. Soil pH in the 0-10 cm soil profile generally had a lower value than in 10-20 cm soil profile. Soil acidification induced by stemflow of C. korshinskii was more intense than that of A. ordosica. Stemflow and throughfall acidification is considered as an important factor resulting in the decrease of soil pH in the direction from the inthershrub spaces to the shrub base.

Key words： stemflow; throughfall; gross rainfall; pH; soil; Caragana korshinskii; Artemisia ordosica

参考文献

[1]Levia D F,Frost E E.A review and evaluation of stemflow literature in the hydrologic and biogeochemical cycles of forested and agricultural ecosystems[J].Journal of Hydrology,2003,274:1-29.

[2]Johnson M S,Lehmann J.Double-funneling of trees:stemflow and root-induced preferential flow[J].Ecoscience,2006,13:324-333.

[3]Navar J,Bryan R.Interception loss and rainfall redistribution by three semi-arid growing near tree trunks in a beechwood on limestone:indications for stemflow induced changes in community structure[J].Applied Soil Ecology,1990,3:115-125.

[4]Crockford R H,Richardson D P.Partitioning of rainfall into throughfall,stemflow and interception:effect of forest type,ground cover and climate[J].Hydrological Processes,2000,14:2903-2920.

[5]王正宁,王新平.荒漠灌丛树干茎流及其入渗、再分配特征[J].中国沙漠,2010,30(5):1108-1113.

[6]马育军,高尚玉,李小雁,等.高寒河谷灌丛冠层降雨再分配特征及影响因素[J].中国沙漠,2012,32(4):963-971.

[7]杨志鹏,李小雁,伊万娟.荒漠灌木树干茎流及其生态水文效应研究进展[J].中国沙漠,2010,30(2):303-311.

[8]Neave M,Abrahams A D.Vegetation influences on water yields from grassland and shrubland ecosystems in the Chihuahuan Desert[J].Earth Surface Processes and Landforms,2002,27:1011-1020.

[9]Herwitz S R.Buttresses of tropical rainforest trees influence hillslope processes[J].Earth Surface Processes and Landforms,1988,13:563-567.

[10]Taniguchi M,Tsujimura M,Tanaka T.Significance of stemflow in groundwater recharge.1.Evaluation of the stemflow contribution to recharge using a mass balance approach[J].Hydrological Processes,1996,10:71-80.

[11]Chang S C,Matzner E.The effect of beech stemflow on spatial patterns of soil solution chemistry and seepage fluxes in a mixed beech/oak stand[J].Hydrological Processes,2000,14:135-144.

[12]Matschonat G,Falkengren-Grerup U.Recovery of soil pH,cation-exchange capacity and the saturation of exchange sites from stemflow-induced soil acidification in three Swedish beech (Fagus sylvatica L.) forests[J].Scandinavian Journal of Forest Research,2000,15:39-48.

[13]Awasthi O P,Sharma E,Palni L M S.Stemflow-a source of nutrients in some naturally growing epiphytic orchids of the Sikkim Himalaya[J].Annals of Botany,1995,75:5-11.

[14]Kaneko N,Kofuji R.Effects of soil pH gradient caused by stemflow acidification on soil microartropod community structure in a Japanese red cedar plantation:an evaluation of ecological risk on decomposition[J].Journal of Forest Research,2000,5:157-162.

[15]Beniamino F,Ponge J F,Arpin P.Soil acidification under the crown of oak trees.1.spatial distribution[J].Forest Ecology and Management,1991,40:221-232.

[16]Satake K,Nakaya K,Takamatsu T.pH distribution in radial sections of the stem and root of Cryptomeria japonica[J].Canadian Journal of Forest Research-Revue,1996,26:503-507.

[17]Finzi A C,Canham C D,Van Breemen N.Canopy tree soil interactions within temperate forests:species effects on pH and cations[J].Ecological Applications,1998,8:447-454.

[18]Fan H B,Hong W,Ma Z,et al.Acidity and chemistry of bulk precipitation,throughfall and stemflow in a Chinese fir plantation in Fujian,China[J].Forest Ecology and Management,1999,122:243-248.

[19]Gersper P L,Holowayc N.Some Effects of stem flow from forest canopy trees on chemical properties of soils[J].Ecology,1971,52:691-702.

[20]刘菊秀,张德强,周国逸,等.鼎湖山酸沉降背景下主要森林类型水化学特征初步研究[J].应用生态学报,2003,14(8):1223-1228.

[21]姚余君,张彦东,任向荣.云杉和落叶松树干径流对土壤pH值的影响[J].东北林业大学学报,2006,34(6):22-25.

[22]Mitchell R J,Truscot A M,Leith I D,et al.A study of the epiphytic communities of Atlantic oak woods along an atmospheric nitrogen deposition gradient[J].Journal of Ecology,2005,93:482-492.

[23]张志山.沙漠人工植被区的生态水文过程[D].北京:中国科学院研究生院,2006.

[24]鲍士旦.土壤农化分析[M].北京:中国农业出版,2000.

[25]Wang X P,Li X R,Zhang J G,et al.Measurement of rainfall interception by xerophytic shrubs in re-vegetated sand dunes[J].Hydrological Sciences Journal,2005,50:897-910.

[26]Duan Z H,Xiao H L,Li X R,et al.Evolution of soil properties on stabilized sands in the Tengger Desert,China[J].Geomorphology,2004,59:237-246.

[27]Andre F,Jonard M,Ponette Q.Effects of biological and meteorological factors on stemflow chemistry within a temperate mixed oak-beech stand[J].Science of the Total Environment,2008,393:72-83.

[28]Levia D F,Herwitz S R.Physical properties of water in relation to stemflow leachate dynamics:implications for nutrient cycling[J].Canadian Journal of Forest Research,2000,30:662-666.

[29]Davie T J A.Fundamentals of Hydrology[M].London:Routledge,2002.

[30]Herwitz S R.Raindrop impact and water flow on the vegetation surfaces of trees and the effect of stemflow and throughfall generation[J].Earth Surface Processes and Landforms,1987,12:425-432.

[31]MartinezMeza E,Whitford W G.Stemflow,throughfall and channelization of stemflow by roots in three Chihuahuan desert shrubs[J].Journal of Arid Environments,1996,32:271-287.

[32]Wang X P,Wang Z N,Berndtsson R,et al.Desert shrub stemflow and its significance in soil moisture replenishment[J].Hydrology and Earth System Sciences,2011,15:561-567.

[33]张志山,樊恒文,赵金龙,等.沙漠人工植物群落的根系分布及动态[J].中国沙漠,2006,26(4):637-643.

[34]Keim R F,Skaugset A E,Weiler M.Storage of water on vegetation under simulated rainfall of varying intensity[J].Advances in Water Resources,2006,29:974-986.

[35]Wang X P,Zhang Y F,Hu R,et al.Canopy storage capacity of xerophytic shrubs in Northwestern China[J].Journal of Hydrology,2012,454/455:152-159.

[36]王正宁.腾格里沙漠东南缘灌丛树干茎流及其生态水文意义[D].北京:中国科学院研究生院,2010.

Options

文章导航

/

〈

〉