Article(id=1261270371689480918, tenantId=1146029695717560320, journalId=1146123166801305609, issueId=1261262687258985194, articleNumber=null, orderNo=null, doi=10.12404/j.issn.1671-1815.2404883, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=research-article, receivedDate=1719676800000, receivedDateStr=2024-06-30, revisedDate=1744300800000, revisedDateStr=2025-04-11, acceptedDate=null, acceptedDateStr=null, onlineDate=1778639889881, onlineDateStr=2026-05-13, pubDate=1752768000000, pubDateStr=2025-07-18, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1778639889881, onlineIssueDateStr=2026-05-13, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1778639889881, creator=13701087609, updateTime=1778639889881, updator=13701087609, issue=Issue{id=1261262687258985194, tenantId=1146029695717560320, journalId=1146123166801305609, year='2025', volume='25', issue='20', pageStart='8317', pageEnd='8759', issueExtLink='null', onlineDate='null', pubDate='null', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=1, issueType=-1, specialIssue=null, createTime=1778638057769, creator=13701087609, updateTime=1778753106634, updator=13701087609, preIssue=null, nextIssue=null, ext={EN=IssueExt(id=1261745237240722095, tenantId=1146029695717560320, journalId=1146123166801305609, issueId=1261262687258985194, language=EN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=), CN=IssueExt(id=1261745237240722096, tenantId=1146029695717560320, journalId=1146123166801305609, issueId=1261262687258985194, language=CN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=)}, issueFiles=null}, startPage=8651, endPage=8658, ext={EN=ArticleExt(id=1261270373379785442, articleId=1261270371689480918, tenantId=1146029695717560320, journalId=1146123166801305609, language=EN, title=Numerical Simulation of Groundwater Dynamics in Sugan Lake Basin Based on MODFLOW, columnId=1156262735643005297, journalTitle=Science Technology and Engineering, columnName=Papers·Hydraulic Engineering, runingTitle=null, highlight=null, articleAbstract=
A numerical simulation of groundwater dynamics in the Sugan Lake Basin was conducted by using MODFLOW, and 50-year predictions were made for four different water diversion schemes. The results from MODFLOW simulations fit well with the measured data, indicating that the established model can be used for predicting the groundwater dynamics in the Sugan Lake Basin. The MODFLOW simulation results under different water diversion schemes reveal that over a period of 50 years, as the amount of diverted water increases, the shrinkage rate of the large Sugan Lake’s area also increases, and the groundwater level in the Sugan Lake Basin shows a general declining trend. The impact of inter-basin water transfer exhibits certain time lags and spatial heterogeneity. Considering both the water diversion requirements and the effects of the water diversion project on the ecological environment of the Sugan Lake Basin, it is suggested that a water diversion scheme of 1.0×108 m3/a is more appropriate. The research results provide important scientific theoretical support for assessing the impacts of inter-basin water transfer projects on the ecological environment of the Sugan Lake Basin and for determining suitable water diversion schemes.
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利用MODFLOW对苏干湖盆地地下水动态进行数值模拟,并对4种不同调水方案进行50年预测。MODFLOW模拟结果与实测情况拟合良好,表明所建模型可用于苏干湖盆地地下水动态的预测。不同调水方案下的MODFLOW模拟结果表明:预测50年时间,随着调水量的增大,大苏干湖面积缩减率随之增大,且苏干湖盆地地下水水位整体呈下降趋势;跨流域调水所产生的影响具有一定的时间滞后性和空间异质性;综合考虑调水需求以及调水工程对苏干湖盆地生态环境的影响,认为调水方案1.0×108 m3/a较为合适。研究成果可为跨流域调水工程对苏干湖盆地生态环境的影响评价以及调水方案的确定提供重要科学理论依据。
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, authorsList=魏新平, 刘兴荣, 王玉昆, 黄金燕, 马彦杰, 李启润)}, authors=[Author(id=1261270381441237820, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, orderNo=0, firstName=null, middleName=null, lastName=null, nameCn=null, orcid=null, stid=null, country=null, authorPic=null, dead=0, email=361819735@qq.com, emailSecond=null, emailThird=null, correspondingAuthor=0, authorType=1, ext={EN=AuthorExt(id=1261270381957137222, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, authorId=1261270381441237820, language=EN, stringName=Xin-ping WEI, firstName=Xin-ping, middleName=null, lastName=WEI, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=
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1 Gansu Institute of Geo-Environment Survey, Lanzhou 730050, China, bio=null, bioImg=null, bioContent=null, aboutCorrespAuthor=null), CN=AuthorExt(id=1261270382103937868, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, authorId=1261270381441237820, language=CN, stringName=魏新平, firstName=null, middleName=null, lastName=null, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=
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1 甘肃省地质环境监测院, 兰州 730050, bio={"content":"
魏新平(1976—),男,汉族,甘肃秦安人,硕士研究生,高级工程师。研究方向:水工环地质调查评价与勘察设计。E-mail: 361819735@qq.com。
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魏新平(1976—),男,汉族,甘肃秦安人,硕士研究生,高级工程师。研究方向:水工环地质调查评价与勘察设计。E-mail: 361819735@qq.com。
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2020., articleTitle=null, refAbstract=null)], funds=[Fund(id=1261270417927487581, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, awardId=23ZDFA009-02, language=CN, fundingSource=甘肃省科技重大专项(23ZDFA009-02), fundOrder=null, country=null), Fund(id=1261270418359500898, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, awardId=2024ZDZX-02, language=CN, fundingSource=甘肃省科学院重大专项(2024ZDZX-02), fundOrder=null, country=null), Fund(id=1261270418602770533, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, awardId=2023ZDYF-03, language=CN, fundingSource=甘肃省科学院重点科技研发项目(2023ZDYF-03), fundOrder=null, country=null)], companyList=[AuthorCompany(id=1261270380912755499, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, xref=1, ext=[AuthorCompanyExt(id=1261270380925338412, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, companyId=1261270380912755499, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
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1 甘肃省地质环境监测院, 兰州 730050)]), AuthorCompany(id=1261270381038584627, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, xref=2, ext=[AuthorCompanyExt(id=1261270381046973236, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, companyId=1261270381038584627, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
2 Institute of Geological Hazards Prevention, Gansu Academy of Sciences, Lanzhou 730000, China), AuthorCompanyExt(id=1261270381055361845, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, companyId=1261270381038584627, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
2 甘肃省科学院地质自然灾害防治研究所, 兰州 730000)])], figs=[ArticleFig(id=1261270401397735430, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=EN, label=Fig.1, caption=
Model area range, figureFileSmall=QXs7/16fCGEpw1VebSlG8Q==, figureFileBig=w0YVoZTHe0SNN8uy4+RhSQ==, tableContent=null), ArticleFig(id=1261270402358231049, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=CN, label=图1, caption=
模型范围, figureFileSmall=QXs7/16fCGEpw1VebSlG8Q==, figureFileBig=w0YVoZTHe0SNN8uy4+RhSQ==, tableContent=null), ArticleFig(id=1261270404753178643, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=EN, label=Fig.2, caption=
Model boundary condition, figureFileSmall=st9EBBtbQDc2vGD5mjfVKA==, figureFileBig=xvAWJ1W1icC9y/oE9rvXsg==, tableContent=null), ArticleFig(id=1261270405147443223, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=CN, label=图2, caption=
模型边界条件, figureFileSmall=st9EBBtbQDc2vGD5mjfVKA==, figureFileBig=xvAWJ1W1icC9y/oE9rvXsg==, tableContent=null), ArticleFig(id=1261270406833553435, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=EN, label=Fig.3, caption=
Hydrogeological parameter zoning graph, figureFileSmall=F7jk8xHg2YShunqm89cdTA==, figureFileBig=UNL/C6b9WxrNoDCSxHqI/A==, tableContent=null), ArticleFig(id=1261270407240400928, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=CN, label=图3, caption=
水文地质参数分区图, figureFileSmall=F7jk8xHg2YShunqm89cdTA==, figureFileBig=UNL/C6b9WxrNoDCSxHqI/A==, tableContent=null), ArticleFig(id=1261270407798243364, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=EN, label=Fig.4, caption=
Fitting graph of groundwater initial flow field measurement and model calculation, figureFileSmall=44kJ6wBGfNmcKW8uc4fZGg==, figureFileBig=XYenb0kvyVjuKVfyWiX+QA==, tableContent=null), ArticleFig(id=1261270408523857959, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=CN, label=图4, caption=
地下水初始流场实测与模型计算拟合图, figureFileSmall=44kJ6wBGfNmcKW8uc4fZGg==, figureFileBig=XYenb0kvyVjuKVfyWiX+QA==, tableContent=null), ArticleFig(id=1261270409022980141, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=EN, label=Fig.5, caption=
The decline of groundwater level in the Sugan Lake Basin at the end of the 50th year under different water transfer scales, figureFileSmall=ba5boVMCVgO99NnewWBz0g==, figureFileBig=pkS6bCNoh0+YK6oEi1E5MA==, tableContent=null), ArticleFig(id=1261270409354330158, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=CN, label=图5, caption=
不同调水规模下苏干湖盆地地下水在第50年末的水位降幅, figureFileSmall=ba5boVMCVgO99NnewWBz0g==, figureFileBig=pkS6bCNoh0+YK6oEi1E5MA==, tableContent=null), ArticleFig(id=1261270409782149169, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=EN, label=Fig.6, caption=
The decline of groundwater level in Sugan Lake Basin at 1.0×108 m3/a in different prediction periods, figureFileSmall=BSkEUIt/iwhOrbMPhfCXxQ==, figureFileBig=ui+efOtTmbir3GfeVZSPfQ==, tableContent=null), ArticleFig(id=1261270411426316340, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=CN, label=图6, caption=
不同预测期苏干湖盆地地下水在调水1.0×108 m3/a时的水位降幅, figureFileSmall=BSkEUIt/iwhOrbMPhfCXxQ==, figureFileBig=ui+efOtTmbir3GfeVZSPfQ==, tableContent=null), ArticleFig(id=1261270411711529015, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=EN, label=Fig.7, caption=
Curves of the relationship between the elevation and storage volume and area of Dasugan Lake, figureFileSmall=LZGHET5Nh1zkT97HWczPdQ==, figureFileBig=xRshuDjd40L95jWMuYWM5w==, tableContent=null), ArticleFig(id=1261270412206456891, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=CN, label=图7, caption=
大苏干湖高程和蓄水量、面积关系曲线, figureFileSmall=LZGHET5Nh1zkT97HWczPdQ==, figureFileBig=xRshuDjd40L95jWMuYWM5w==, tableContent=null), ArticleFig(id=1261270412391006269, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=EN, label=Fig.8, caption=
Variation curve of water area of Dasugan Lake under different watertransfer scales, figureFileSmall=an3Xi85abc8IxgIK/UTJGQ==, figureFileBig=yNwDZqhdJ3loNeGUW8Fp9w==, tableContent=null), ArticleFig(id=1261270412676218944, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=CN, label=图8, caption=
不同调水规模下大苏干湖水域面积变化曲线, figureFileSmall=an3Xi85abc8IxgIK/UTJGQ==, figureFileBig=yNwDZqhdJ3loNeGUW8Fp9w==, tableContent=null), ArticleFig(id=1261270412881739846, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=EN, label=Table 1, caption=
Hydrogeological parameter zoning
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| 分区 | 水文地质参数 |
| 渗透系数K/(m·d-1) | 给水度μ |
| Ⅰa | 4.30 | 0.15 |
| Ⅰb | 118.00 | 0.25 |
| Ⅰc | 63.12 | 0.25 |
| Ⅰd | 28.23 | 0.25 |
| Ⅰe | 18.98 | 0.20 |
), ArticleFig(id=1261270413112426568, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=CN, label=表1, caption=
水文地质参数分区
, figureFileSmall=null, figureFileBig=null, tableContent=
| 分区 | 水文地质参数 |
| 渗透系数K/(m·d-1) | 给水度μ |
| Ⅰa | 4.30 | 0.15 |
| Ⅰb | 118.00 | 0.25 |
| Ⅰc | 63.12 | 0.25 |
| Ⅰd | 28.23 | 0.25 |
| Ⅰe | 18.98 | 0.20 |
), ArticleFig(id=1261270413229867084, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=EN, label=Table 2, caption=
Identification equilibrium and measured equilibrium comparison
, figureFileSmall=null, figureFileBig=null, tableContent=
| 指标 | 模拟值/ (104 m3·a-1) | 实际值/ (104 m3·a-1) | 变化 率/% |
| 侧向径流流入 | 101 11.42 | 10 111.42 | 0 |
| 大哈尔腾河入渗 | 32 800.00 | 32 800.00 | 0 |
| 小哈尔腾河入渗 | 6 900.00 | 6 900.00 | 0 |
| 补给项 | 当中泉-努呼图区降水入渗 | 271.53 | 271.53 | 0 |
| 苏干湖区降水入渗 | 1 253.46 | 1 253.46 | 0 |
| 泉水入渗(重复量) | 15 222.59 | 14 921.25 | 2.02 |
| 合计 | 51 336.42 | 51 336.42 | 0 |
| 排泄项 | 当中泉-努呼图区潜水蒸发 | 4 303.62 | 4 272.01 | 0.74 |
| 苏干湖区潜水蒸发 | 27 479.03 | 27 763.46 | -1.02 |
| 大苏干湖水面蒸发 | 17 420.91 | 17 079.27 | 2.00 |
| 小苏干湖水面蒸发 | 2 018.40 | 2 018.40 | 0 |
| 当中泉-努呼图区泉水溢出 | 15 222.59 | 14 921.25 | 2.02 |
| 苏干湖区泉水溢出 | 17 420.91 | 17 079.27 | 2.00 |
| 侧向径流流出 | 50.00 | 50.00 | 0 |
| 合计 | 51 271.06 | 51 183.14 | 0.17 |
), ArticleFig(id=1261270413364084814, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=CN, label=表2, caption=
识别均衡与实测均衡对比
, figureFileSmall=null, figureFileBig=null, tableContent=
| 指标 | 模拟值/ (104 m3·a-1) | 实际值/ (104 m3·a-1) | 变化 率/% |
| 侧向径流流入 | 101 11.42 | 10 111.42 | 0 |
| 大哈尔腾河入渗 | 32 800.00 | 32 800.00 | 0 |
| 小哈尔腾河入渗 | 6 900.00 | 6 900.00 | 0 |
| 补给项 | 当中泉-努呼图区降水入渗 | 271.53 | 271.53 | 0 |
| 苏干湖区降水入渗 | 1 253.46 | 1 253.46 | 0 |
| 泉水入渗(重复量) | 15 222.59 | 14 921.25 | 2.02 |
| 合计 | 51 336.42 | 51 336.42 | 0 |
| 排泄项 | 当中泉-努呼图区潜水蒸发 | 4 303.62 | 4 272.01 | 0.74 |
| 苏干湖区潜水蒸发 | 27 479.03 | 27 763.46 | -1.02 |
| 大苏干湖水面蒸发 | 17 420.91 | 17 079.27 | 2.00 |
| 小苏干湖水面蒸发 | 2 018.40 | 2 018.40 | 0 |
| 当中泉-努呼图区泉水溢出 | 15 222.59 | 14 921.25 | 2.02 |
| 苏干湖区泉水溢出 | 17 420.91 | 17 079.27 | 2.00 |
| 侧向径流流出 | 50.00 | 50.00 | 0 |
| 合计 | 51 271.06 | 51 183.14 | 0.17 |
), ArticleFig(id=1261270413984841811, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=EN, label=Table 3, caption=
Statistics of area change rate of Dasugan Lake under different water transfer scales
, figureFileSmall=null, figureFileBig=null, tableContent=
预测时 间/年 | 不同调水规模下大苏干湖面积变化率/% |
调水规模 为0.8× 108 m3/a | 调水规模 为0.9× 108 m3/a | 调水规模 为1.0× 108 m3/a | 调水规模 为1.2× 108 m3/a |
| 5 | -0.22 | -0.36 | -0.32 | -0.55 |
| 10 | -0.94 | -1.35 | -1.27 | -2.02 |
| 20 | -2.25 | -3.35 | -3.45 | -4.99 |
| 30 | -3.83 | -4.91 | -5.05 | -7.44 |
| 50 | -5.48 | -7.31 | -7.51 | -10.67 |
), ArticleFig(id=1261270417738743897, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1261270371689480918, language=CN, label=表3, caption=
不同调水规模下大苏干湖面积变化率统计
, figureFileSmall=null, figureFileBig=null, tableContent=
预测时 间/年 | 不同调水规模下大苏干湖面积变化率/% |
调水规模 为0.8× 108 m3/a | 调水规模 为0.9× 108 m3/a | 调水规模 为1.0× 108 m3/a | 调水规模 为1.2× 108 m3/a |
| 5 | -0.22 | -0.36 | -0.32 | -0.55 |
| 10 | -0.94 | -1.35 | -1.27 | -2.02 |
| 20 | -2.25 | -3.35 | -3.45 | -4.99 |
| 30 | -3.83 | -4.91 | -5.05 | -7.44 |
| 50 | -5.48 | -7.31 | -7.51 | -10.67 |
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