Journal of Hydrology-Regional Studies最新文献

{"title":"Multi-objective synergy and competition relationship of water and sediment regulation of the Heishanxia reservoir in upstream of the Yellow River Basin","authors":"","doi":"10.1016/j.ejrh.2024.102045","DOIUrl":"10.1016/j.ejrh.2024.102045","url":null,"abstract":"<div><h3>Study region</h3><div>Heishanxia Reservoir, upstream of the Yellow River Basin.</div></div><div><h3>Study focus</h3><div>The complicated management of the Yellow River Basin stems primarily from an uncoordinated relationship between water and sediment. The un-built Heishanxia Reservoir has been designated as one of seven pivotal projects, and its regulating effect remains to be thoroughly studied. First, nine typical inflow water and sediment scenarios were constructed based on probability inference. Then, a multi-objective water and sediment regulation model of Heishanxia Reservoir was established with the objectives of maximum erosion quantity (EQ) of the channel, maximum ecological satisfaction rate (ESR), and maximum power generation (PG). Finally, the multi-dimensional regulating effect was revealed, and the synergy-competition relationships among EQ, ESR and PG were analyzed.</div></div><div><h3>New hydrological insights for the region</h3><div>The operation of Heishanxia can increase the discharge during the flood season in the downstream Ning-Meng Channel, and the average annual EQ is 0.19×10⁸ t more than the current condition. Further, the ESR decreases slightly during the high-flow and normal-flow years and increases slightly during the low-flow years. The PG in the upper reaches of the Yellow River has increased by approximately 10 %. Among the three objectives, EQ and ESR, as well as EQ and PG, demonstrate a competitive relationship, whereas ESR and PG exhibit a synergistic relationship. Reservoir inflow plays a major role in the changes of synergy-competition relationship.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":null,"pages":null},"PeriodicalIF":4.7,"publicationDate":"2024-10-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142561254","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Hydro-chemical tracers and hydro-chemical modeling assessing groundwater leakage for a karst aquifer in Yarkon-Taninim basin, Israel","authors":"","doi":"10.1016/j.ejrh.2024.102033","DOIUrl":"10.1016/j.ejrh.2024.102033","url":null,"abstract":"<div><h3>Study region</h3><div>Yarkon-Taninim groundwater basin, Israel.</div></div><div><h3>Study focus</h3><div>A Paleocene-Eocene thermal episode caused an anomaly of barium and silica concentrations in the Eocene aquitard that were used as natural tracers for identifying and quantifying leakage into the Turonian – Upper Cenomanian aquifer through the Senonian-Paleocene (Mount-Scopus Group) strata. Increased concentrations of both Ba²⁺ and SiO₂ in Turonian – Upper Cenomanian aquifer groundwater were supposed to be a sign of downward leakage from the Eocene aquitard. Within the Menashe syncline where these tracers pointed to the leakage, it was estimated by the balance method. Using this estimate, the area-averaged hydraulic conductivity of the intermedium layer was assessed from the Darcy’s law by using this layer thickness and a hydraulic gradient between the Avdat-Group aquitard and the Turonian – Upper Cenomanian aquifer. The calculation and integration of its results over the balance area by a grid with 1×1 km² cells was performed by using the GIS-based ARGUS ONE software. Cl^- and SO₄^2- concentrations in the leakage have been estimated by using the mixing model considering the assessed leakage. PHREEQC software was used for solubility calculation of amorphous silica, quartz and barite at different temperatures, pH and salinities and for calculation of saturation indices of Ba-bearing minerals.</div></div><div><h3>New hydrological insights for the region</h3><div>Previously the Senonian layers within synclines in the Yarkon-Taninim basin, which is the primary source of the groundwater supply in Israel, were supposed to be impermeable. This study has shown that the main leakage is concentrated in the Menashe syncline vicinity north of the Yarkon-Taninim basin. The two tracers first provided a possibility of the leakage assessment within the Menashe syncline: more than 2.3*10⁶ – 11.4*10⁶ m³ yr⁻¹ (leakage rate of 5.4*10⁻⁵ – 2.6*10⁻⁴ m day⁻¹ at the Eocene outcrops of the syncline). The average regional permeability of the Senonian aquiclude within the Menashe syncline was estimated in the range 7.7*10⁻⁵ – 3.8*10⁻⁴ m day⁻¹, essentially higher as compared to the values for the Bet-Govrin syncline. The salinity of the slow leakage was assessed to be low; therefore, it will not damage the high-quality groundwater in the Turonian – Upper Cenomanian aquifer that is exploited for the potable water supply.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":null,"pages":null},"PeriodicalIF":4.7,"publicationDate":"2024-10-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142538712","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Machine learning modeling reveals the spatial variations of lake water salinity on the endorheic Tibetan Plateau","authors":"","doi":"10.1016/j.ejrh.2024.102042","DOIUrl":"10.1016/j.ejrh.2024.102042","url":null,"abstract":"<div><h3>Study region</h3><div>The endorheic Tibetan Plateau (TP).</div></div><div><h3>Study focus</h3><div>Water salinity is sensitive indicator for variations of lake hydrologic and physicochemical characteristics. Due to the heterogeneous influences from geographical and climatic factors, lake water salinity is highly sensitive to environmental diversity and changes. The TP hosts a wide distribution of lakes, the majority of which belong to endorheic drainage type and are saline or salty lakes. However, the harsh environment on the TP poses great challenges for the in<strong>–</strong>site measurements at large scales, impeding the comprehension of the pattern and variations of lake water salinity across the TP.</div></div><div><h3>New hydrological insights for the region</h3><div>Benefiting extensive field surveys and a meta–analysis, this study establishes machine learning models based on measurements from 100 terminal lakes (&gt;1 km²) and related physical variables. The optimal model (R² = 0.90, MAE = 8.11 g/L, MAPE = 36.40 %, RMSE = 12.51 g/L, RRMSE = 36.96 g/L) is then applied to predict the water salinity of the other 214 unmeasured terminal lakes. The modeling results reveal a spatial variation pattern of increasing water salinity of these terminal lakes from south to north across the endorheic basins. Further classification of water salinity levels indicated that more than half (213) of the terminal lakes are in an oligosaline state. This study contributes to a spatially–explicit understanding of the distribution variations in water salinity of terminal TP lakes and provides a feasible approach for estimating water salinity of unmeasured lakes at large scales.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":null,"pages":null},"PeriodicalIF":4.7,"publicationDate":"2024-10-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142538713","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"The role of automated surface water distribution systems in energy-saving agriculture: A case study from central Iran’s Arid Plateau","authors":"","doi":"10.1016/j.ejrh.2024.102036","DOIUrl":"10.1016/j.ejrh.2024.102036","url":null,"abstract":"<div><h3>Study region</h3><div>The NekooAbad Irrigation District in central Iran faces challenges due to inefficient surface water distribution. 82 million m³ of groundwater is extracted annually from 15,000 tube-wells, leading to decreased groundwater levels and increased energy consumption of 234 million kWh per year.</div></div><div><h3>Study focus</h3><div>This study explores implementing automation in surface water distribution to reduce groundwater extraction and conserve energy. A hydraulic simulation model and a centralized Model Predictive Control approach were used to analyze the existing system and propose a recovery plan. The potential impact of automated surface water distribution on reducing groundwater extraction and energy conservation was evaluated through spatial assessment in GIS.</div></div><div><h3>New hydrological insights for the region</h3><div>The results demonstrate that the introduction of automation can significantly improve surface water distribution and, accordingly, groundwater overexploitation and, consequently, energy conservation, particularly during water scarcity. Energy conservation increased by 42.3 %, 54.8 %, 56.2 %, and 57.7 % under normal conditions, with water shortages of less than 10 %, 10–15 %, and 15–20 %, respectively. However, as the surface water shortages intensified, the energy conservation rates decreased to 57.7 %, 43.7 %, 25.4 %, and 18.9 % for normal conditions, water shortages of 15–20 %, 20–30 %, 30–40 %, and over 40 %, respectively. The automation introduction effectively provided reliable surface water resources, prompting farmers to shut down pumping stations or reduce working hours. Even in extreme scenarios, the project achieved up to 18.9 % energy savings.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":null,"pages":null},"PeriodicalIF":4.7,"publicationDate":"2024-10-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142538714","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Simplified spatially distributed, coupled soil moisture–groundwater model, evaluated for Flanders (Belgium)","authors":"","doi":"10.1016/j.ejrh.2024.102006","DOIUrl":"10.1016/j.ejrh.2024.102006","url":null,"abstract":"<div><h3>Study region</h3><div>Flanders region of Belgium.</div></div><div><h3>Study focus</h3><div>In hydrological studies, there is a need for computationally fast, spatially distributed models involving the unsaturated zone soil moisture, groundwater and their interactions, while maintaining good accuracy. This study builds on an approach based on the AquaCrop model for the unsaturated zone and a 2D explicit groundwater flow model. The model’s speed stems from its simplicity, while AquaCrop’s wide use provides a basic database for parameterization.</div><div>Capillary rise, often not (explicitly) assessed in distributed models, is considered. For coupling the unsaturated and saturated zones better, the capillary rise algorithm by AquaCrop was modified. Groundwater flow to the rivers is represented combining Darcy’s law and the linear reservoir concept. Surface runoff modelling is modified to better incorporate the effects of urban environments. The model was parameterized using publicly available data (involving minimal calibration) and tested for Flanders.</div></div><div><h3>New hydrological insights for the region</h3><div>Despite its simplicity, the model often performed acceptably. Its accuracy was generally higher for the degree of saturation in the upper 70 cm of the soil (R=0.90, RMSE=0.14) than the first 10 cm (R=0.68, RMSE=0.17). The groundwater levels for wells with observed depths less than 5 m were simulated better (R=0.82, RMSE=0.72 m) than the deeper ones (R=0.63, RMSE=4.59 m). Capillary rise was found to be a potentially substantial source of water to the crops.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":null,"pages":null},"PeriodicalIF":4.7,"publicationDate":"2024-10-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142535041","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Compound effects of sea level and flow on river-induced flooding in coastal areas of southern Sweden","authors":"","doi":"10.1016/j.ejrh.2024.102032","DOIUrl":"10.1016/j.ejrh.2024.102032","url":null,"abstract":"<div><h3>Study region</h3><div>Rönne River, Säve River, and Höje River, Sweden.</div></div><div><h3>Study focus</h3><div>River-induced flooding in coastal areas results from a multitude of drivers interacting in complex ways. The primary drivers are sea level (SL) and river flow (Q) that often exhibit coherent behavior to be considered in flood risk management. To describe and quantify the compound effects of SL and Q on flooding, a methodology was developed involving hydraulic simulations with long time series of data yielding statistical properties of output quantities such as river water level and flooded areas. Dominance analysis was conducted to quantify the relative influence of SL and Q on river water level along reaches. Also, simplified, empirically based equations were derived to predict the river water level at any location based on SL and Q<strong>.</strong></div></div><div><h3>New hydrological insights for the region</h3><div>The long-term simulations revealed that the relative influence of SL and Q on the river water level changes significantly from the coast to upstream. For example, at the Rönne River, influence of SL decreases from 90 % to 20 % between 1 km and 11 km from the coast. Meanwhile, influence of Q increases from 10 % to 80 % over the same distance. The simplified equations derived to predict the water level can be used by stakeholders to forecast flood events or in risk assessment where many alternatives need to be considered.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":null,"pages":null},"PeriodicalIF":4.7,"publicationDate":"2024-10-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142535040","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Runoff simulation of the Kaidu River Basin based on the GR4J-6 and GR4J-6-LSTM models","authors":"","doi":"10.1016/j.ejrh.2024.102034","DOIUrl":"10.1016/j.ejrh.2024.102034","url":null,"abstract":"<div><h3>Study region</h3><div>The Kaidu River Basin originates from the southern slope of the Tienshan Mountains in the Xinjiang Uygur Autonomous Region, China.</div></div><div><h3>Study focus</h3><div>Accurate runoff simulation and prediction significantly affect flood control, drought resilience, and water resource allocation decisions. This study establishes the GR4J-6 model (modèle du Génie Rural à 4 paramètres Journalier-6, including a snowmelt module) and integrates it with the LSTM (Long Short-Term Memory) model to construct the hybrid GR4J-6-LSTM model and enhance the simulation accuracy of snowmelt runoff. A case study is conducted in the Kaidu River Basin to demonstrate the applicability of these models in cold and arid regions. The accuracy of the GR4J-6, LSTM, and GR4J-6-LSTM models is evaluated using Nash-Sutcliffe efficiency (NSE), Kling-Gupta Efficiency (KGE), and Root Mean Squared Error (RMSE) metrics. In addition, the contributions of each feature variable in the models are analyzed using the SHapley Additive exPlanations (SHAP) method to enhance the reliability of the results.</div></div><div><h3>New hydrological insights for the region</h3><div>The GR4J-6 model demonstrated good applicability in the Kaidu River Basin, with NSE, KGE, and RMSE values of 0.69, 0.79, and 39.39 m³/s during the validation period, respectively. The hybrid model GR4J-6-LSTM exhibited the highest comprehensive accuracy among all the models, with NSE, KGE, and RMSE values of 0.84, 0.87, and 28.79 m³/s, respectively. In the LSTM model, temperature and precipitation were found to significantly influence the simulated runoff, indicating that higher temperature and precipitation lead to increased runoff. In the GR4J-6-LSTM model, Tmin (minimum temperature) and the hydrological feature variable Qsim exhibited a strong positive correlation with simulated runoff, as Tmin and Qsim increased, they promoted stronger flow production. This study provides a framework for runoff simulation in snowmelt river basins, offering a reference for projecting extreme hydrological events under climate change.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":null,"pages":null},"PeriodicalIF":4.7,"publicationDate":"2024-10-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142535039","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Characterization of drought propagation over the Tibetan Plateau","authors":"","doi":"10.1016/j.ejrh.2024.102035","DOIUrl":"10.1016/j.ejrh.2024.102035","url":null,"abstract":"<div><h3>Study region</h3><div>This study was carried out on the Tibetan Plateau (TP), which contains multiple important ecosystems, is the source of many rivers in China, and is experiencing significant climate change.</div></div><div><h3>Study focus</h3><div>Clarifying drought propagation characteristics is crucial for understanding the mechanism of drought development and benefiting drought mitigation and early warning schemes. However, there is currently a notable lack of research on droughts on the TP and drought propagation characteristics on the TP have yet to be investigated. In this study, we investigated drought propagation time, probability, threshold, and the climatic factors associated with drought development based on the copula probability model and correlation, Bayesian network, and attribution analyses, allowing us to fill current research gaps.</div></div><div><h3>New hydrological insights for the region</h3><div>The research framework proposed in this study effectively reflected the characteristics of drought propagation. Our results showed that seasonality and aridity controlled the propagation time from meteorological drought (MD) to agricultural drought (AD), i.e., the time was shortest in summer (2.3<img>11.0 months) and in the humid zone (2.3<img>7 months); the same pattern was found for the propagation of MD to hydrological drought (HD), with the propagation time being 2.3<img>3.0 months in summer and 2.3<img>6 months in humid zones. The propagation probability for both AD and HD generally increased synchronously with the severity of MD, and also exhibited seasonal patterns, with the highest probability values in summer (0.59<img>0.90 for AD and 0.51<img>0.82 for HD). The highest propagation thresholds were also found in summer (−1.68 to −1.09 for AD and −1.68 to −1.36 for HD). The trends of both propagation time and probability were significant, and the probability of HD exhibited significant downward trends (−0.074 to −0.030/decade) across the TP. Precipitation was the dominant factor controlling the development of drought in most cases; however, other climatic factors, such as maximum temperature, solar radiation, and specific humidity, contributed 14.0 %<img>43.9 % of the variances of AD and HD.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":null,"pages":null},"PeriodicalIF":4.7,"publicationDate":"2024-10-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142534454","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Satellite observations of surface water dynamics and channel migration in the Yellow River since the 1980s","authors":"","doi":"10.1016/j.ejrh.2024.102029","DOIUrl":"10.1016/j.ejrh.2024.102029","url":null,"abstract":"<div><h3>Study region</h3><div>the Yellow <em>River</em> (YR) in China.</div></div><div><h3>Study focus</h3><div>Due to climate <em>change</em> and human activities, YR channel morphology has undergone significant spatiotemporal variations. Yet, a comprehensive understanding of channel migration in YR and its driving factors remains unclear. Here, we developed a multi-index water extraction method to track the changes in surface water and river channel migration of YR based on Landsat imagery since the 1980s.</div></div><div><h3>New hydrological insights for the region</h3><div>We find that the <em>average</em> surface water area of YR over the past four decades is 4013 km², with 73.5 % of permanent surface water. Notably, the surface water extent has experienced a 9 % increase since the 1980s, while the river channel has undergone a 12.2 % decrease. The YR channel’s centerline exhibits diverse change patterns across the entire basin, which can be broadly categorized into six types ranging from unchanged to reverse migration. We identify that climate, particularly temperature and precipitation, contributed 71 % of channel changes in the upper reaches, while 65 % of changes in the lower reaches are from human activities, including reservoir operations and water management policies. Our results unveil the variations in water extent and channel migration of the YR, offering new insights into the interactions between channel migration and climate change and human activities in the YR over the past four decades.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":null,"pages":null},"PeriodicalIF":4.7,"publicationDate":"2024-10-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142534452","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Evaluation of the source and mechanisms of groundwater recharge for the southern sections of the western Afar rift margin and associated rift floor","authors":"","doi":"10.1016/j.ejrh.2024.102037","DOIUrl":"10.1016/j.ejrh.2024.102037","url":null,"abstract":"<div><h3>Study area</h3><div>Southern Sections of Western Afar rift margin and associated rift floor<em>.</em></div></div><div><h3>Study focus</h3><div>The purpose of this study is to identify the source and mechanisms of groundwater recharge based on geological, hydrochemical, and environmental isotope studies.</div></div><div><h3>New hydrogeological insights</h3><div>The investigation illustrate that the columnar jointed basalt was extended from the plateau to the rift margin. In addition, transverse structures trending NW-SE and NE-SW connect the plateau to the rift margin and the marginal grabens to the rift floor. The hydrochemical interpretations with EC and TDS shows that the groundwater from the plateau has evolved from Ca-dominated and slightly mineralized to Na-dominated and highly mineralized to the rift floor. Isotopically, the deep groundwater systems are depleted in the entire physiography in contrast to the shallow groundwater systems. Radon measurements are higher at the outlets of the marginal grabens and between the rift margin and the rift floor, suggesting groundwater feeds the river. A comprehensive analysis of the aforementioned results suggests that the deep circulating groundwater is recharged in the plateau and escarpment and chemically altered with increasing depth and along its preferential flow path into the rift floor. Therefore, the plateau area is the main source of recharge for the western Afar rift margin and associated rift floor, due to the presence of preferential pathways, mainly the columnar jointed basalts and cross-structures.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":null,"pages":null},"PeriodicalIF":4.7,"publicationDate":"2024-10-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142534453","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}