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JOURNAL OF DESERT RESEARCH  2014, Vol. 34 Issue (1): 60-66    DOI: 10.7522/j.issn.1000-694X.2013.00286
    
Influences of Flooding on Degraded Riparian Vegetation along the Lower Tarim River
Fu Jinyi1,2, Xu Hailiang1, Zhao Xinfeng1, Bai Yuan1,2, Wang Xiyi1,2
1. Key Laboratory of Oasis Ecology and Desert Environment, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China;
2. University of Chinese Academy of Sciences, Beijing 100049, China
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Abstract  A study was carried out to investigate the effects of flooding on the riparian vegetation in moderately, severely and extremely degraded area along the Lower Tarim River, by analyzing the community structure and diversity of the riparian vegetation under different degradation degrees. The results showed that: (1) In the three degraded areas, the life forms in non-flooding sampling plots were trees and shrubs with the species percentages of 62.5%, 100% and 75%, respectively. The plant life forms in flooding sampling plots in moderately and severely degraded areas were perennial herbs with the species percentages of 37.5% and 42.86%, and the life form in extremely degraded area was still tree and shrub after flooding with the species percentage of 50%. (2) Impacted by flooding disturbance, the dominant species of the three degraded areas changed from trees and shrubs to perennial herbs and annual herbs. (3) Compared with the non-flooding sampling plots, the Simpson indices of the flooding ones in the three degraded areas increased by 40.55%, 66.24% and 171.39%, respectively. The Shannon-Wiener indices of the flooding ones in the three degraded areas increased by 42.75%, 72.68% and 197.6%, respectively. The Margalef indices of the flooding ones in three degraded areas increased by 105.98%, 88.54% and 120.88%, respectively. Therefore, the extremely degraded area had the most apparent increase of diversity indices impacted by flooding disturbance.
Key words:  riparian vegetation      degraded area      flooding disturbance      Tarim River     
Received:  24 December 2012      Published:  20 January 2014
ZTFLH:  Q948.11  
Corresponding Authors:  徐海量,xuhl@ms.xjb.ac.cn     E-mail:  xuhl@ms.xjb.ac.cn

Cite this article: 

Fu Jinyi, Xu Hailiang, Zhao Xinfeng, Bai Yuan, Wang Xiyi. Influences of Flooding on Degraded Riparian Vegetation along the Lower Tarim River. JOURNAL OF DESERT RESEARCH, 2014, 34(1): 60-66.

URL: 

http://www.desert.ac.cn/EN/10.7522/j.issn.1000-694X.2013.00286     OR     http://www.desert.ac.cn/EN/Y2014/V34/I1/60

[1] 王新平,张志山,张景光,等.荒漠植被影响土壤水文过程研究述评[J].中国沙漠,2005,25(2):196-201.
[2] 康尔泗,陈仁升,张智慧,等.内陆河流域水文过程研究的一些科学问题[J].地球科学进展,2007,22(9):940-953.
[3] Bischoff A.Dispersal and establishment of floodplain grassland species as limiting factors in restoration[J].Biological Conservation,2002,104:25-33.
[4] 李吉玫,徐海量,张占江,等.河水漫溢对塔里木河下游荒漠河岸林地表植被与土壤种子库的影响[J].应用生态学报,2008,19(8):1651-1657.
[5] Valett H M,Baker M A,Morrice J A,et al.Biogeochemical and metabolic responses to the flood pulse in a semiarid floodplain[J].Ecology,2005,86:220-234.
[6] Ubugunov L L,Ubugunova V I.Soils of floodplains in arid regions of Inner Asia (the Zavkhan River,Mongolia)[J].Eurasian Soil Science,2012,45(3):237-245.
[7] 周斌,杨红梅,胡顺军,等.河水漫溢对塔里木河下游土壤及植被的影响[J].干旱区地理,2010,33(3):442-448.
[8] Jolly I D,Walker G R,Thorburn P J.Salt accumulation in semi-arid floodplain soils with implications for forest health[J].Journal of Hydrology,150(2/4):589-614.
[9] James C S,Capon S,White M G,et al.Spatial variability of the soil seed bank in a heterogeneous ephemeral wetland system in semi-arid Australia[J].Plant Ecology,2007,190:205-217.
[10] Capon S J,Brock M A.Flooding,soil seed bank dynamics and vegetation resilience of a hydrologically variable desert floodplain[J].Freshwater Biology,2005,51(2):206-223.
[11] Jensen A E.The role of seed banks and soil moisture in recruitment of semi-arid floodplain plants:the River Murray Australia[D].Adelaide,Australia:University of Adelaide,2008.
[12] Capon S J.Plant community responses to wetting and drying in a large arid floodplain[J].River Research and Applications,2003,19:509-520.
[13] Tiegs S D,OLeary J F,Pohl M M,et al.Flood disturbance and riparian species diversity on the Colorado River Delta[J].Biodiversity and Conservation,2005,14:1175-1194.
[14] 陈永金,陈亚宁,刘加珍.塔里木河下游植被覆盖度变化与地下水质关系[J].环境科学,2010,31(3):612-617.
[15] 邓潮州,张希明,李利,等.塔里木河下游胡杨群落特征及种群结构分析[J].中国沙漠,2010,30(3):589-595.
[16] 王增如,徐海量,尹林克,等.塔里木河下游荒漠化过程土壤种子库特征[J].中国沙漠,2009,29(5):885-890.
[17] 马克平,黄建辉,于顺利,等.北京东灵山地区植物群落多样性的研究Ⅱ丰富度、均匀度和物种多样性指数[J].生态学报,1995,15(3):268-277.
[18] 郝兴明,陈亚宁,李卫红.新疆塔里木河下游物种多样性与地下水位的关系[J].生态学报,2007,27(10):4106-4112.
[19] 鲁庆彬,游卫云,赵昌杰,等.旅游干扰对青山湖风景区植物多样性的影响[J].应用生态学报,2011,22(2):295-302.
[20] 王振锡,潘存德,石鑫鑫.胡杨年轮记录的塔里木河下游54年来区域水环境历史变迁[J].生态环境学报,2010,19(3):637-645.
[21] 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.
[22] 陈亚宁,张宏锋,李卫红,等.新疆塔里木河下游物种多样性变化与地下水位的关系[J].地球科学进展,2005,20(2):158-165.
[23] 崔艳,王新平,冯丽,等.天然固定沙地与人工固沙植被区土壤种子库的比较研究[J].中国沙漠,2010,30(5):1114-1119.
[24] 李秋艳,赵文智.干旱区土壤种子库的研究进展[J].地球科学进展,2005,20(3):350-358.
[25] 王增如,徐海量,尹林克,等.塔里木河下游植被退化区土壤种子库特征[J].干旱区资源与环境,2008,22(9):143-148.
[26] 李卫红,徐海量,艾合买提·那尤甫.塔里木河下游输水与生态恢复监测初报[J].干旱区地理,2003,26(2):122-128.
[27] 王让会,卢新民,宋郁东,等.西部干旱区生态需水的规律及特点——以塔里木河下游绿色走廊为例[J].应用生态学报,2003,14(4):520-524.
[28] 叶朝霞,陈亚宁,李卫红.基于生态水文过程的塔里木河下游植被生态需水量研究[J].地理学报,2007,62(5):451-461.
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