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[1]WANG Juan,ZHANG Fei,YU Haiyang,et al.Analysis on the Hydrological and Ecological Characteristics Based on the LUCC in Weigan and Kuqa River[J].Research of Soil and Water Conservation,2016,23(02):236-242.

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Analysis on the Hydrological and Ecological Characteristics Based on the LUCC in Weigan and Kuqa River

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 23 Number of periods: 2016 02 Page number: 236-242 Column: Public date: 2016-04-28

Title:: Analysis on the Hydrological and Ecological Characteristics Based on the LUCC in Weigan and Kuqa River

Author(s):: WANG Juan^1,2,3, ZHANG Fei^1,2,3, YU Haiyang^1,2,3, REN Yan^1,2,3, ZHANG Yue^1,2,3; 1. College of Resources and Environment Science, Xinjiang University, Urumqi 830046, China;
2. Key Laboratory of oasis Ecology, Xinjiang University, Urumqi 830046, China;
3. Key Laboratory of Xinjiang wisdom city and environment modeling Urumqi, Urumqi 830046, China

Keywords:: LUCC; hydrological; ecological; maximum likelihood classification

CLC:: X87

DOI:: -

Abstract:: Land use/land cover change (LUCC) is one of the core issues in global change research. Because of human behaviors, especially the aggravated land utilization by wasteland cultivation, more fertilizer and land utilization change resulting from cosmically disafforestation and disintegrating habit, the nature landscape was seriously destroyed and the survival environment of animals and plants was inflected, which degrade the eco-system function. As a result, high intensity of human activity let LUCC has the great influence on the hydrosphere and biosphere. We used the typical oasis Weigan-kuqa River as the study area. We used the method of maximum likelihood for image classification and statistics of cultivated land, forest land, saline land, water, and the bare land in the years of 1989, 1998, 2013. The results show that:(1) from the aspects of hydrological, LUCC changed significantly because of the human activities in the oasis Weigan-kuqa Rive, from 1989 to 2013, in total, cultivated area increased by 2.408×10³ km² that led to irrigation and other water consumption, at the same time, combination of construction of irrigation channels and reservoirs and other activities promoted increased surface runoff and caused the decline of underground water level year by year; (2) from the aspects of ecological, LUCC caused climate change with the main factors of human activity in the study area, it was caused by changes in temperature, humidity and evaporation, with the widespread increase of arable land, grassland and woodland area decreased to some extent, making the biodiversity simple and simplex significantly. Therefore, study on the characteristics of hydrological and ecological as well as environmental impacts and mechanisms based on the LUCC has the significant scientific value.

References:: [1] 郝仕龙,李春静.黄土丘陵区土地利用/覆盖变化对生态承载力的影响:以固原上黄试验区为例[J].水土保持研究,2013,20(2):135-138.
[2] 宋戈,李娜,李静,等.建三江垦区土地利用/覆盖变化与生态环境效应作用机理研究[J].经济地理,2011,31(5):816-821.
[3] Baird A J, Wilby R L. Eco-hydrology:plants and water in terrestrial and aquatic environments[M]. UK, Hove:Psychology Press, 1999.
[4] Tighe Matthew, Haling Rebecca E, Flavel Richard J, et al. Ecological succession, hydrology and carbon acquisition of biological soil crusts measured at the micro-scale[J]. PLoS ONE,2012,7(10):e48565.
[5] Daniel L. Peters, Wendy A. Monk, Donald J. Baird. Cold-regions Hydrological Indicators of Change(CHIC)for ecological flow needs assessment[J]. Hydrological Sciences Journal,2014,59(3/4):502-516.
[6] Peters Daniel L, Baird Donald J, Monk Wendy A, et al. Establishing standards and assessment criteria for ecological instream flow needs in agricultural regions of Canada[J]. Journal of Environmental Quality,2012,41(1):41-51.
[7] 李崇巍,刘世荣,孙鹏森,等.岷江上游景观格局及生态水文特征分析[J].生态学报,2005,25(4):691-698.
[8] 黄青.塔里木河中游景观格局与生态水文过程的耦合分析[J].干旱区资源与环境,2008,22(9):83-87.
[9] 叶柏生,杨大庆,丁永建,等.中国降水观测误差分析及其修正[J].地理学报,2007,62(1):3-13.
[10] Gao X, Ye B S, Zhang S Q, et al. Glacier runoff variation and its influence on river runoff during1961-2006 in the Tarim River Basin, China[J]. Science China:Earth Scinece,2010,40(6):654-665.
[11] 陈小兵,杨劲松,乔晓英,等.绿洲耕地适宜面积确定与减灾研究:以新疆渭干河灌区为例[J].中国地质灾害与防治学报,2008,19(1):118-123.
[12] 邓书斌. ENVI遥感图像处理方法[M].北京:科学出版社,2010.
[13] 梅安新,彭望琭,秦其明,等.遥感导论[M].北京:高等教育出版社,2001.
[14] 方炫,安韶山,薛志婧,等.基于最大似然与矩法的黄土高原小流域土壤碳氮空间变异分析[J].水土保持通报,2014,34(4):141-146.
[15] 孙倩,塔西甫拉提·特依拜,张飞,等.渭干河-库车河三角洲绿洲土地利用/覆被时空变化遥感研究[J].生态学报,2012,32(10):3252-3265.
[16] 程国栋,肖洪浪,徐中民,等.中国西北内陆河水问题及其应对策略:以黑河流域为例[J].冰川冻土,2006,28(3):406-413.
[17] 严登华,王浩,杨舒媛,等.干旱区流域生态水文耦合模拟与调控的若干思考[J].地球科学进展,2008,23(7):773-778.
[18] 付梦娣,妙旭华,全占军,等.庆阳市土地利用变化的景观生态效应研究[J].水土保持研究,2014,21(6):241-244.
[19] 王凌河,严登华,龙爱华,等.流域生态水文过程模拟研究进展[J].地球科学进展,2009,24(8):891-898.
[20] 丁永建,叶柏生,韩添丁,等.过去50 a中国西部气候和径流变化的区域差异[J].中国科学D辑:地球科学,2007,37(2):206-214.
[21] 李珍,姜逢清.1961-2004年新疆气候突变分析[J].冰川冻土,2007,29(6):351-359.
[22] 王钧,蒙吉军.黑河流域近60 a来径流量变化及影响因素[J].地理科学,2008,28(1):83-88.
[23] 闫金凤,陈曦.绿洲浅层地下水位与水质变化对人为驱动LUCC的响应:以三工河流域为例[J].自然资源学报,2005,20(2):172-180.
[24] 邓伟,何岩.论地下水对地表生态的作用[J].地理科学,1993,13(2):161-168.
[25] 满苏尔·沙比提,陈冬花.渭干河-库车河三角洲绿洲形成演变和可持续发展研究[J].资源科学,2005,27(6):118-124.
[26] 黄秉维,郑度,赵名茶,等.现代自然地理[M].北京:科学出版社,1999.
[27] Sala O E, Chapin F S, Armesto J J, et al. Biodiversity-Global biodiversity scenarios for the year 2100[J]. Science,2011,287(5459):1770-1774.
[28] Noss R F, Quigley H B, Hornocker M G, et al. Conservation biology and carnivore conservation in the Rocky Mountains[J]. Conservation Biology, 1996,10(4):949-963.
[29] 满苏尔·沙比题,陈冬花.渭干河-库车河三角洲绿洲形成演变和可持续发展研究[J].资源科学,2005,27(6):118-124.
[30] 董淼,王雪梅,席瑞,等.渭干河-库车河三角洲绿洲土地利用/覆盖结构变化及荒漠化响应[J].天津农业科学,2014,20(3):40-43.

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