{"title":"空间异质性对沿海含水层地下坝上游残盐水去除的影响","authors":"Jun Wang, Jun Kong, Chao Gao","doi":"10.1002/hyp.70222","DOIUrl":null,"url":null,"abstract":"<div>\n \n <p>Although subsurface dams can effectively control seawater intrusion, the trapped saltwater behind the dam significantly impedes groundwater resource utilisation. Previous studies have largely neglected the impact of spatial heterogeneity on residual saltwater desalination processes. To address this research gap, this study provides the first field-scale simulation of how spatial heterogeneity and connectivity features influence the mechanism and timescale of residual saltwater removal. The results show that under certain conditions, <i>Tr</i> (timescale of residual saltwater removal) in heterogeneous aquifers varies by approximately −69% to 145% relative to <i>Tr</i> in homogeneous aquifers. Although spatial heterogeneity and connectivity features significantly change the time-varying course of residual saltwater removal rate, they do not alter the mechanism of residual saltwater removal. Additionally, in homogeneous scenarios, <i>Tr</i> increases with the increase of dam height or decrease of dam distance from the sea boundary (dam location). In heterogeneous aquifers, <i>Tr</i> maintains a significant positive correlation with dam height under isotropic conditions; however, this relationship does not necessarily hold under anisotropic conditions. Regardless of heterogeneity types, there is no significant relationship between <i>Tr</i> and dam location. Sensitivity analyses demonstrate a non-monotonic relationship between <i>Tr</i> and three key heterogeneity parameters: (i) the variance of logarithmic hydraulic conductivity (<span></span><math>\n <semantics>\n <mrow>\n <msubsup>\n <mi>σ</mi>\n <mi>Y</mi>\n <mn>2</mn>\n </msubsup>\n </mrow>\n <annotation>$$ {\\sigma}_Y^2 $$</annotation>\n </semantics></math>), (ii) vertical correlation length (<span></span><math>\n <semantics>\n <mrow>\n <msubsup>\n <mi>δ</mi>\n <mi>Y</mi>\n <mi>υ</mi>\n </msubsup>\n </mrow>\n <annotation>$$ {\\delta}_Y^{\\upsilon } $$</annotation>\n </semantics></math>), and (iii) anisotropy ratio (<i>anis</i>). Further analysis shows that, in general, <i>Tr</i> is more sensitive to <span></span><math>\n <semantics>\n <mrow>\n <msubsup>\n <mi>σ</mi>\n <mi>Y</mi>\n <mn>2</mn>\n </msubsup>\n </mrow>\n <annotation>$$ {\\sigma}_Y^2 $$</annotation>\n </semantics></math>, <span></span><math>\n <semantics>\n <mrow>\n <msubsup>\n <mi>δ</mi>\n <mi>Y</mi>\n <mi>υ</mi>\n </msubsup>\n </mrow>\n <annotation>$$ {\\delta}_Y^{\\upsilon } $$</annotation>\n </semantics></math>, and <i>anis</i> in aquifers with multivariate Gaussian structures compared to those containing either connected high-<i>K</i> structures or connected low-<i>K</i> structures. These results highlight the importance of spatial heterogeneity, including connectivity features, in assessing timescale of residual saltwater removal, which is valuable for protecting of coastal groundwater resources.</p>\n </div>","PeriodicalId":13189,"journal":{"name":"Hydrological Processes","volume":"39 8","pages":""},"PeriodicalIF":2.9000,"publicationDate":"2025-08-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Impacts of Spatial Heterogeneity on Residual Saltwater Removal Upstream of Subsurface Dams in Coastal Aquifers\",\"authors\":\"Jun Wang, Jun Kong, Chao Gao\",\"doi\":\"10.1002/hyp.70222\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div>\\n \\n <p>Although subsurface dams can effectively control seawater intrusion, the trapped saltwater behind the dam significantly impedes groundwater resource utilisation. Previous studies have largely neglected the impact of spatial heterogeneity on residual saltwater desalination processes. To address this research gap, this study provides the first field-scale simulation of how spatial heterogeneity and connectivity features influence the mechanism and timescale of residual saltwater removal. The results show that under certain conditions, <i>Tr</i> (timescale of residual saltwater removal) in heterogeneous aquifers varies by approximately −69% to 145% relative to <i>Tr</i> in homogeneous aquifers. Although spatial heterogeneity and connectivity features significantly change the time-varying course of residual saltwater removal rate, they do not alter the mechanism of residual saltwater removal. Additionally, in homogeneous scenarios, <i>Tr</i> increases with the increase of dam height or decrease of dam distance from the sea boundary (dam location). In heterogeneous aquifers, <i>Tr</i> maintains a significant positive correlation with dam height under isotropic conditions; however, this relationship does not necessarily hold under anisotropic conditions. Regardless of heterogeneity types, there is no significant relationship between <i>Tr</i> and dam location. Sensitivity analyses demonstrate a non-monotonic relationship between <i>Tr</i> and three key heterogeneity parameters: (i) the variance of logarithmic hydraulic conductivity (<span></span><math>\\n <semantics>\\n <mrow>\\n <msubsup>\\n <mi>σ</mi>\\n <mi>Y</mi>\\n <mn>2</mn>\\n </msubsup>\\n </mrow>\\n <annotation>$$ {\\\\sigma}_Y^2 $$</annotation>\\n </semantics></math>), (ii) vertical correlation length (<span></span><math>\\n <semantics>\\n <mrow>\\n <msubsup>\\n <mi>δ</mi>\\n <mi>Y</mi>\\n <mi>υ</mi>\\n </msubsup>\\n </mrow>\\n <annotation>$$ {\\\\delta}_Y^{\\\\upsilon } $$</annotation>\\n </semantics></math>), and (iii) anisotropy ratio (<i>anis</i>). Further analysis shows that, in general, <i>Tr</i> is more sensitive to <span></span><math>\\n <semantics>\\n <mrow>\\n <msubsup>\\n <mi>σ</mi>\\n <mi>Y</mi>\\n <mn>2</mn>\\n </msubsup>\\n </mrow>\\n <annotation>$$ {\\\\sigma}_Y^2 $$</annotation>\\n </semantics></math>, <span></span><math>\\n <semantics>\\n <mrow>\\n <msubsup>\\n <mi>δ</mi>\\n <mi>Y</mi>\\n <mi>υ</mi>\\n </msubsup>\\n </mrow>\\n <annotation>$$ {\\\\delta}_Y^{\\\\upsilon } $$</annotation>\\n </semantics></math>, and <i>anis</i> in aquifers with multivariate Gaussian structures compared to those containing either connected high-<i>K</i> structures or connected low-<i>K</i> structures. These results highlight the importance of spatial heterogeneity, including connectivity features, in assessing timescale of residual saltwater removal, which is valuable for protecting of coastal groundwater resources.</p>\\n </div>\",\"PeriodicalId\":13189,\"journal\":{\"name\":\"Hydrological Processes\",\"volume\":\"39 8\",\"pages\":\"\"},\"PeriodicalIF\":2.9000,\"publicationDate\":\"2025-08-26\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Hydrological Processes\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://onlinelibrary.wiley.com/doi/10.1002/hyp.70222\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"Environmental Science\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Hydrological Processes","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1002/hyp.70222","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"Environmental Science","Score":null,"Total":0}
引用次数: 0
摘要
虽然地下坝可以有效控制海水入侵,但大坝后的滞留盐水严重阻碍了地下水资源的利用。以往的研究在很大程度上忽略了空间异质性对剩余海水淡化过程的影响。为了弥补这一研究空白,本研究首次在野外尺度上模拟了空间异质性和连通性特征对剩余盐水去除机制和时间尺度的影响。结果表明,在一定条件下,非均质含水层残余盐水去除时间尺度Tr变化约为−69% to 145% relative to Tr in homogeneous aquifers. Although spatial heterogeneity and connectivity features significantly change the time-varying course of residual saltwater removal rate, they do not alter the mechanism of residual saltwater removal. Additionally, in homogeneous scenarios, Tr increases with the increase of dam height or decrease of dam distance from the sea boundary (dam location). In heterogeneous aquifers, Tr maintains a significant positive correlation with dam height under isotropic conditions; however, this relationship does not necessarily hold under anisotropic conditions. Regardless of heterogeneity types, there is no significant relationship between Tr and dam location. Sensitivity analyses demonstrate a non-monotonic relationship between Tr and three key heterogeneity parameters: (i) the variance of logarithmic hydraulic conductivity ( σ Y 2 $$ {\sigma}_Y^2 $$ ), (ii) vertical correlation length ( δ Y υ $$ {\delta}_Y^{\upsilon } $$ ), and (iii) anisotropy ratio (anis). Further analysis shows that, in general, Tr is more sensitive to σ Y 2 $$ {\sigma}_Y^2 $$ , δ Y υ $$ {\delta}_Y^{\upsilon } $$ , and anis in aquifers with multivariate Gaussian structures compared to those containing either connected high-K structures or connected low-K structures. These results highlight the importance of spatial heterogeneity, including connectivity features, in assessing timescale of residual saltwater removal, which is valuable for protecting of coastal groundwater resources.
Impacts of Spatial Heterogeneity on Residual Saltwater Removal Upstream of Subsurface Dams in Coastal Aquifers
Although subsurface dams can effectively control seawater intrusion, the trapped saltwater behind the dam significantly impedes groundwater resource utilisation. Previous studies have largely neglected the impact of spatial heterogeneity on residual saltwater desalination processes. To address this research gap, this study provides the first field-scale simulation of how spatial heterogeneity and connectivity features influence the mechanism and timescale of residual saltwater removal. The results show that under certain conditions, Tr (timescale of residual saltwater removal) in heterogeneous aquifers varies by approximately −69% to 145% relative to Tr in homogeneous aquifers. Although spatial heterogeneity and connectivity features significantly change the time-varying course of residual saltwater removal rate, they do not alter the mechanism of residual saltwater removal. Additionally, in homogeneous scenarios, Tr increases with the increase of dam height or decrease of dam distance from the sea boundary (dam location). In heterogeneous aquifers, Tr maintains a significant positive correlation with dam height under isotropic conditions; however, this relationship does not necessarily hold under anisotropic conditions. Regardless of heterogeneity types, there is no significant relationship between Tr and dam location. Sensitivity analyses demonstrate a non-monotonic relationship between Tr and three key heterogeneity parameters: (i) the variance of logarithmic hydraulic conductivity (), (ii) vertical correlation length (), and (iii) anisotropy ratio (anis). Further analysis shows that, in general, Tr is more sensitive to , , and anis in aquifers with multivariate Gaussian structures compared to those containing either connected high-K structures or connected low-K structures. These results highlight the importance of spatial heterogeneity, including connectivity features, in assessing timescale of residual saltwater removal, which is valuable for protecting of coastal groundwater resources.
期刊介绍:
Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.