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  • CN 62-1070/P
  • ISSN 1000-694X
  • Bimonthly 1981
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Relation of Dominant Herbaceous Plant Species to Groundwater Depth in the Lower Reaches of Tarim River

  • Wang Xiyi ,
  • Xu Hailiang ,
  • Pan Cunde ,
  • Ling Hongbo ,
  • Zhang Pei
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  • 1. Xinjiang Agricultural University, Urumqi 830052;
    2. Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China

Received date: 2014-09-23

  Revised date: 2014-12-09

  Online published: 2016-01-20

Abstract

By conducting field investigation of the herbaceous community characteristics in lower reaches of the Tarim River and combined with the groundwater depth data, this paper discussed the relationship between groundwater depth and characteristics of herbaceous. The results revealed that: (1)with the increase of groundwater depth, the biodiversity and coverage of herbaceous presented a decreasing trend, and the ecological structure tended to be simple; The composition and species diversity of herbaceous were relatively high where the groundwater depth shallower than 6 m, while, fewer herbaceous plant distributed where the groundwater depth deeper than 7 m. (2)At large scale space, the distributed characteristics of herbaceous along with groundwater depth was in agreement with other desert region, i.e. as the groundwater depth increased, the order of succession was Phragmites Adans community with high water level, Glossogyne tenuifolia community with medium water level, Alhagi sparsif community with lower water level; there were otherness, similarity, and continuity among the herbaceous community corresponding to different groundwater depth. (3)The ecological niche width of advantage herbaceous species was not wide in the lower reaches of Tarim River, due to the restriction of water environmental conditions; while the ecological niche width of Phragmites communis and Alhagi sparsif, which were widely distributed, wider than others. To sum up, groundwater depth was the key factor which affected the species composition and type of herbaceous.

Cite this article

Wang Xiyi , Xu Hailiang , Pan Cunde , Ling Hongbo , Zhang Pei . Relation of Dominant Herbaceous Plant Species to Groundwater Depth in the Lower Reaches of Tarim River[J]. Journal of Desert Research, 2016 , 36(1) : 216 -224 . DOI: 10.7522/j.issn.1000-694X.2014.00195

References

[1] 孙儒泳,李博,诸葛阳,等.普通生态学[M].北京:高等教育出版社,1993:121-130.
[2] Jack B,Abraham M,Gideon O. Economic development of groundwater in arid zones with applications to the Negev Desert,Israel[J].Management Science,1994,40(3):353-363.
[3] Lan D J,Kerryn L M,Kate L H.A review of groundwater surface water interactions in arid/semi-arid wetlands and the consequences of salinity for wetland ecology[J].Ecohydrology,2008,1(1):43-58.
[4] 汤奇成,张捷斌.西北干旱地区水资源与生态环境保护[J].地理科学进展,2001,20(3):227-233.
[5] 徐海量,宋郁东,王强,等.塔里木河中下游地区不同地下水位对植被的影响[J].植物生态学报,2004,28(3):400-405.
[6] 冯起.荒漠绿洲植被生长与地下水位的研究[J].中国沙漠,1998,18(增刊):107-109.
[7] 王水献,吴彬,杨鹏年,等.焉耆盆地绿洲灌区生态安全下的地下水埋深合理界定[J].资源科学,2011,33(3):422-430.
[8] Andrew J B,Robert L.Eco-Hydrology-Plants and Water in Terrestrial and Aquatic Environments[M].London,UK:Routledge,1999:57-61.
[9] 赵文智,常学礼,李启森,等.荒漠绿洲区芦苇种群构建生物量与地下水埋深关系[J].生态学报,2003,23(6):1138-1146.
[10] Burke A.Classification and ordination of plant communities of the Naukluft mountains,Namibia[J].Journal of Vegetation Science,2001,12:53-60.
[11] 江洪,黄建辉,陈灵芝,等.东灵山植物群落的排序、数量分类与环境解释[J].植物学报,1994,36(7):539-551.
[12] 张金屯.植被数量生态学方法[M].北京:中国科学技术出版社,1995:217-226.
[13] 张峰,张金屯,张峰.历山自然保护区猪尾沟森林群落植被格局及环境解释[J].生态学报,2003,23(3):421-427.
[14] Tongway D J,Ludwig J A.Small-scale resource heterogeneity in semi-arid landscapes[J].Pacific Conservation Biology,1994,1:201-208.
[15] Michael R,Zhang X M.Ecophysiology and habitat requirements of perennial plant species in the Taklimakan Deser[M].Aachen,Germany:ShakerVerlag,2004:1-35.
[16] Reda A,Robert R,Tao W,et al.Groundwater quality and management in arid and semi-arid regions:case study,Central Eastern Desert of Egypt[J].Journal of African Earth Sciences,2012,69(6):13-25.
[17] Felipe O,Parikshit V,Steven P,et al.Monitoring and modeling water-vegetation interactions in groundwater-dependent ecosystems[J].Reviews of Geophysics,2012,50(3):1-24.
[18] 金晓媚,胡光成,史晓杰.银川平原土壤盐渍化与植被发育和地下水埋深关系[J].现代地质,2009,23(1):23-27.
[19] 安乐生,赵全升,叶思源,等.黄河三角洲地下水关键水盐因子及其植被效应[J].水科学进展,2011.22(5):689-695.
[20] 马玉蕾,王德,刘俊民,等.黄河三角洲典型植被与地下水埋深和土壤盐分的关系[J].应用生态学报,2013,24(9):2423-2430.
[21] 赵成义,王玉朝,李保国.内陆河流域植被变化与地下水运动的耦合关系[J].水利学报,2003,48(12):59-65.
[22] 郑丹,李卫红,陈亚鹏,等.干旱区地下水与天然植被关系研究综述[J].资源科学,2005,27(4):160-167.
[23] 苏里坦,宋郁东,张展羽,等.天山北麓地下水与自然植被的空间变异及其分形特征[J].山地学报,2005,23(1):14-20.
[24] 黄金廷,侯光才,尹立河,等.干旱半干旱区天然植被的地下水水文生态响应研究[J].干旱区地理,2011.34(5):788-793.
[25] 樊自立,马英杰,张宏,等.塔里木河流域生态地下水位及其合理深度确定[J].干旱区地理,2004,27(1):8-13.
[26] 郝兴明,陈亚宁,李卫红,等.塔里木河中下游荒漠河岸林植被对地下水埋深变化的响应[J].地理学报,2008,63(11):1123-1130.
[27] 房世波,谭凯炎,刘建栋,等.鄂尔多斯植被盖度分布与环境因素的关系[J].植物生态学报,2009,33(1):25-33.
[28] 王希义,徐海量,凌红波,等.塔里木河中游荒漠河岸林物种多样性对地下水埋深变化的响应[J].西北植物学报,2013,33(10):2071-2076.
[29] 徐海量,陈亚宁,杨戈.塔里木河下游生态输水对植被和地下水位的影响[J].环境科学,2003,24(4):18-22.
[30] 朱成刚,李卫红,马建新,等.塔里木河下游地下水位对柽柳叶绿素荧光特性的影响[J].应用生态学报,2010,21(7):1689-1696.
[31] 安红燕,徐海量,叶茂,等.塔里木河下游胡杨径向生长与地下水的关系[J].生态学报,2011,31(8):2053-2059.
[32] 黄粤,包安明,王士飞,等.间歇性输水影响下的2001-2011年塔里木河下游生态环境变化[J].地理学报,2013,68(9):1251-1262.
[33] 宋郁东,樊自立,雷志栋,等.中国塔里木河水资源与生态问题研究[M].乌鲁木齐:新疆人民出版社,2000:37-41.
[34] 钱亦兵,周华荣,赵锐锋,等.塔里木河中下游湿地及其周边土壤理化性状的空间异质性[J].水土保持学报,2005,19(6):31-34.
[35] 张平,吴昊,殷洪建,等.颗粒级配对毛细水上升影响的研究[J].节水灌溉,2010,35(7):24-26.
[36] 陈亚宁,李卫红,徐海量,等.塔里木河下游地下水位对植被的影响[J].地理学报,2003,58(4):542-549.
[37] 郝兴明,陈亚宁,李卫红,等.胡杨根系水力提升作用的证据及其生态学意义[J].植物生态学报,2009,33(6):1125-1131.
[38] 苏芮,李卫红,郝兴明,等.荒漠河岸林地区胡杨幼苗根系水力提升作用探究[J].干旱区研究,2012,29(2):342-346.
[39] Yu T F,Feng Q,Si J H,et al.Patterns,magnitude,and controlling factors of hydraulic redistribution of soil water by Tamarix ramosissima roots[J].Journal of Arid Land,2013,5(3):396-407.
[40] Jaccard P.The distribution of the flora in the alpine zone[J].New Phytologist,1912,11(2):37-50.
[41] 赵文智,刘鹄.荒漠区植被对地下水埋深响应研究进展[J].生态学报,2006,26(8):2702-2708.
[42] Levens R.Evolution in Changing Environments:Some Theoretical Explorations[M].Princeton,USA:Princeton University Press,1968:25-31.
[43] Nash M S,Wierenga P J,Butler N A.Variation intension,water content,and drainage rate along a 91 m transect[J].Soil Science,1989,148(2):94-101.
[44] Yuan S F,Chen Y N,Li W H,et al.Analysis of the aboveground biomass and spatial distribution of shrubs in the lower reaches of Tarim River,Xinjiang,China[J].Acta Ecologica Sinica,2006,26(6):1818-1824.
[45] Hill M O.Reciprocal averaging,an eigenvector method of ordination[J].Journal of Ecology,1973,61:237-249.
[46] Robbins B D,Bell S S.Dynamicsofa subtidal seagrass landscape:seasonal and annual change in relation towater depth[J].Ecology,2000,81(5):1193-1205.
[47] 张桂莲,张金屯.关帝山神尾沟优势种生态位分析[J].武汉植物学研究,2002,20(3):203-208.
[48] 李向义,林丽莎,赵强.策勒绿洲外围不同地下水埋深下主要优势植物的分布和群落特征[J].干旱区地理,2009,32(6):906-911.
[49] 朱军涛,于静洁,王平,等.额济纳荒漠绿洲植物群落的数量分类及其与地下水环境的关系分析[J].植物生态学报,2011,35(5):480-489.
[50] 吉久昌,郭跃东,郭晋平,等.文峪河上游河岸林群落类型及其生态适应性[J].生态学报,2009,29(3):1587-1595.
[51] 张绘芳,李霞,王建刚,等.塔里木河下游植物群落结构特征分析[J].生态环境,2007,16(4):1219-1224.
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