Please wait a minute...
干旱区科学
  Research Articles 本期目录 | 过刊浏览 | 高级检索 |
Two-way coupling of unsaturated-saturated flow by integrating the SWAT and MODFLOW models with application in an irrigation district in arid region of West China
Yi LUO, Marios SOPHOCLEOUS
1 Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China; 2 Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; 3 Kansas Geological Survey, University of Kansas, Lawrence, Kansas 66047, USA
Two-way coupling of unsaturated-saturated flow by integrating the SWAT and MODFLOW models with application in an irrigation district in arid region of West China
Yi LUO, Marios SOPHOCLEOUS
1 Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China; 2 Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; 3 Kansas Geological Survey, University of Kansas, Lawrence, Kansas 66047, USA
下载:  PDF (340KB) 
输出:  BibTeX | EndNote (RIS)      
摘要 This paper presents the realization of two-way coupling of the unsaturated-saturated flow interactions of the SWAT2000 and MODFLOW96 models on the basis of the integrated surface/groundwater model SWATMOD99, and its application in Hetao Irrigation District (HID), Inner Mongolia, China. Major revisions and enhancements were made to the SWAT2000 and MODFLOW models for simulating the detailed hydrologic budget and coupled unsaturated and saturated interactions, and irrigation canal hydrology for the HID. The simulation results of seasonal groundwater recharge to and evaporate from the shallow groundwater, and the annual water budget over the district are presented and discussed. The results implied the necessity of two-way coupling of the unsaturated-saturated interactions when groundwater is shallow, and the feasibility of making comprehensive use of the information coming from both the surface water and groundwater models to make a more physically-based assessment of the coupled interactions.
服务
把本文推荐给朋友
加入引用管理器
E-mail Alert
RSS
作者相关文章
Yi LUO
Marios SOPHOCLEOUS
关键词:  Holocene  climate variation  lake level  lake sediment  arid environment    
Abstract: This paper presents the realization of two-way coupling of the unsaturated-saturated flow interactions of the SWAT2000 and MODFLOW96 models on the basis of the integrated surface/groundwater model SWATMOD99, and its application in Hetao Irrigation District (HID), Inner Mongolia, China. Major revisions and enhancements were made to the SWAT2000 and MODFLOW models for simulating the detailed hydrologic budget and coupled unsaturated and saturated interactions, and irrigation canal hydrology for the HID. The simulation results of seasonal groundwater recharge to and evaporate from the shallow groundwater, and the annual water budget over the district are presented and discussed. The results implied the necessity of two-way coupling of the unsaturated-saturated interactions when groundwater is shallow, and the feasibility of making comprehensive use of the information coming from both the surface water and groundwater models to make a more physically-based assessment of the coupled interactions.
Key words:  Holocene    climate variation    lake level    lake sediment    arid environment
收稿日期:  2011-03-28      修回日期:  2011-04-11           出版日期:  2011-09-07      发布日期:  2011-09-07      期的出版日期:  2011-09-07
基金资助: National Basic Research Program of China (2010CB951002); Knowledge Innovation Project of Chinese Academy of Sciences (KZXC2-YW-BR-12)
通讯作者:  Yi LUO    E-mail:  luoyi.cas@hotmail.com
引用本文:    
Yi LUO, Marios SOPHOCLEOUS. Two-way coupling of unsaturated-saturated flow by integrating the SWAT and MODFLOW models with application in an irrigation district in arid region of West China[J]. 干旱区科学, 10.3724/SP.J.1227.2011.00164.
Yi LUO, Marios SOPHOCLEOUS. Two-way coupling of unsaturated-saturated flow by integrating the SWAT and MODFLOW models with application in an irrigation district in arid region of West China. Journal of Arid Land, 2011, 3(3): 164-173.
链接本文:  
http://jal.xjegi.com/CN/10.3724/SP.J.1227.2011.00164  或          http://jal.xjegi.com/CN/Y2011/V3/I3/164
[1] LIU Bing, JIN Heling, SUN Zhong, ZHAO Shuang. Geochemical weathering of aeolian sand and its palaeoclimatic implications in the Mu Us Desert, northern China, since the Late Holocene[J]. 干旱区科学, 2016, 8(5): 647-659.
[2] SHI Peihong, YANG Taibao, TIAN Qingchun, LI Chengxiu. A warmer but drier Marine Isotope Stage 11 during the past 650 ka as revealed by the thickest loess on the western Chinese Loess Plateau[J]. 干旱区科学, 2016, 8(3): 315-330.
[3] WAN Honglian, HUANG Chunchang, PANG Jiangli. Major elements in the Holocene loess-paleosol sequence in the upper reaches of the Weihe River valley, China[J]. 干旱区科学, 2016, 8(2): 197-206.
[4] HAO Xingming, LI Weihong . Oasis cold island effect and its influence on air temperature: a case study of Tarim Basin, Northwest China[J]. 干旱区科学, 2016, 8(2): 172-183.
[5] WU Huawu, LI Xiaoyan, LI Jing, JIANG Zhiyun, LI Guangyong, LIU Lei. Evaporative enrichment of stable isotopes (δ18O and δD) in lake water and the relation to lake-level change of Lake Qinghai, Northeast Tibetan Plateau of China[J]. 干旱区科学, 2015, 7(5): 623-635.
[6] Jeff B LANGMAN. Spatial distribution of δ2H and δ18O values in the hydrologic cycle of the Nile Basin[J]. 干旱区科学, 2015, 7(2): 133-145.
[7] Zhi ZHANG, ZhiBao DONG, ChangZhen YAN, GuangYin HU. Change of lake area in the southeastern part of China’s Badain Jaran Sand Sea and its implications for recharge sources[J]. 干旱区科学, 2015, 7(1): 1-9.
[8] Yu LI, NaiAng WANG, ChengQi ZHANG, Yue WANG. Early Holocene environment at a key location of the northwest boundary of the Asian summer monsoon: a synthesis on chronologies of Zhuye Lake, Northwest China[J]. 干旱区科学, 2014, 6(5): 511-528.
[9] DongWei GUI, FanJiang ZENG, Zhen LIU, Bo ZHANG. Root characteristics of Alhagi sparsifolia seedlings in response to water supplement in an arid region, northwestern China[J]. 干旱区科学, 2013, 5(4): 542-551.
[10] SongHao SHANG. Lake surface area method to define minimum ecological lake level from level–area–storage curves[J]. 干旱区科学, 2013, 5(2): 133-142.
[11] Long MA, JingLu WU, Jilili Abuduwaili. The climatic and hydrological changes and environmental responses recorded in lake sediments of Xinjiang, China[J]. 干旱区科学, 2011, 3(1): 1-8.
No Suggested Reading articles found!
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed