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Source distribution, ecological risks, and controlling factors of heavy metals in river sediments: Receptor model-based study in a transboundary river basin 河流沉积物中重金属的来源分布、生态风险及控制因素——基于受体模型的跨界河流流域研究
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-02-01 DOI: 10.1016/j.ijsrc.2024.10.001
Abu Reza Md Towfiqul Islam , Abu Hena Md Fazla Rabbi , Amit Hasan Anik , Rahat Khan , Md Abdullah Al Masud , Grara Nedjoud , Abubakr M. Idris , Md Naimur Rahman , Venkatramanan Senapathi
In the context of transboundary rivers, which constitute intricate fluvial ecosystems, the persistent threat of heavy metals (HMs) contamination poses significant risks to ecosystem health. In this study, ecotoxicological hazards, governing factors, and the distribution of nine HMs (uranium (U), lead (Pb), cadmium (Cd), nickel (Ni), chromium (Cr), manganese (Mn), iron (Fe), zinc (Zn), and copper (Cu)), as well as sediment characteristics (sand, silt, clay, organic matter, and pH) are assessed within the sediment. The current investigation encompasses the analysis of twenty-seven sediment samples, utilizing inductively coupled plasma mass spectrometry, in the transboundary river basin of Bangladesh, specifically the Teesta River. Notably, the findings underscore the predominance of Cd as a contaminant, responsible for 51.85%, 81.84%, and 100% of the geo-accumulation index, contamination factor, and enrichment factor, respectively. The Teesta River emerges as moderately to highly polluted, with cumulative probabilities of 7.4%, 85.2%, and 7.4% denoting “medium”, “high”, and “priority” pollution levels, respectively. Regions in the upstream and downstream middle sections of the study area exhibit relatively higher pollution levels, particularly in proximity to Kaunia Upazila in the Rangpur district. Ecologically, the potential risk index indicates a low likelihood of ecological impacts at 77.8%, alongside a moderate risk observation of 22.2%. The current results attribute the distribution of these HMs to the pH and organic matter content within the sediment, serving as pivotal factors. To unravel the origins of the HMs, the positive matrix factorization (PMF) model successfully identifies four contributing factors, primarily from geogenic sources. Validation of the PMF model through Spearmen correlation and principal component analysis (PCA) reveals a consistent pattern, affirming its efficacy in this analysis. Within the region, HM sources are identified as originating from anthropogenic activities such as irrigation, industrial discharges, and domestic effluent, in addition to substantial inputs from geogenic sources. Recognizing the transboundary nature of metal pollution, the current study underscores the imperative for continuous and vigilant monitoring, coupled with the implementation of robust management practices. The interplay of both anthropogenic and geogenic factors necessitates a comprehensive approach to effectively and sustainably combat HM contamination.
就构成复杂河流生态系统的跨界河流而言,重金属污染的持续威胁对生态系统健康构成重大风险。在本研究中,评估了9种重金属(铀(U)、铅(Pb)、镉(Cd)、镍(Ni)、铬(Cr)、锰(Mn)、铁(Fe)、锌(Zn)和铜(Cu))在沉积物中的生态毒理学危害、控制因素和沉积物特征(砂、粉、粘土、有机质和pH)。目前的调查包括利用电感耦合等离子体质谱法对孟加拉国跨界河流流域,特别是蒂斯塔河的27个沉积物样本进行分析。值得注意的是,研究结果强调了Cd作为污染物的优势,分别占地质累积指数、污染因子和富集因子的51.85%、81.84%和100%。Teesta河呈现中度至重度污染,累积概率分别为7.4%,85.2%和7.4%,分别表示“中度”,“高度”和“优先”污染水平。研究区中上游和下游区域的污染水平相对较高,特别是在Rangpur地区的Kaunia Upazila附近。在生态方面,潜在风险指数显示低生态影响的可能性为77.8%,中度风险观测值为22.2%。目前的结果将这些HMs的分布归因于沉积物中的pH和有机质含量,这是关键因素。为了揭示HMs的起源,正矩阵分解(PMF)模型成功地识别了四个主要来自地质来源的影响因素。通过spearman相关和主成分分析(PCA)对PMF模型进行了验证,发现了一致的模式,证实了PMF模型在本分析中的有效性。在该区域内,HM来源被确定为源自人为活动,如灌溉、工业排放和家庭污水,以及大量来自地质来源的输入。认识到金属污染的跨界性质,目前的研究强调必须进行持续和警惕的监测,同时实施强有力的管理做法。人为因素和地质因素的相互作用需要一个全面的方法来有效和可持续地对抗HM污染。
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引用次数: 0
Flash floods on the northern coast of the Black Sea: Formation and characteristics 黑海北部海岸的山洪:形成与特征
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-02-01 DOI: 10.1016/j.ijsrc.2024.10.003
Ludmila Kuksina , Pelagiya Belyakova , Valentin Golosov , Ekaterina Zhdanova , Maxim Ivanov , Anatoly Tsyplenkov , Artem Gurinov
Flash floods are one of the most dangerous hydrometeorological events in the world. The current study investigates flash floods on the northern Black Sea Coast. The data about stochastic and relatively stable factors of flash flood formation (such as hydrological, meteorological, lithological, geomorphological, and anthropogenic parameters) were collected for 22 events. The main trigger of flash floods is heavy rainfall of high intensity in the region but in some cases flash flood occurrence is connected with combinations of several “non-critical” factors. The small watershed area (≤351 km2) of river basins experiencing flash floods promotes very rapid flow concentration. Analysis of extreme precipitation demonstrates significant increasing trends in river basins on the Crimean Peninsula and decreasing a maximum precipitation amount in 5 days (r5d) and 1 day (r1d) in river basins in the Caucasus Black Sea Coast in the 21st century as determined by processing of Integrated Multi-satellite Retrievals for Global precipitation measurement (IMEGR) satellite data. At the same time land network data indicates increasing r5d at the Anapa and r1d at the Tuapse meteorological stations in 1961–2020. More frequent occurrence of flash floods has been suggested in the area due to statistical analysis of the longest precipitation ranges. The main reason for significant social and economic damage is uncontrolled human activity in flooded areas on the northern Black Sea Coast.
山洪暴发是世界上最危险的水文气象事件之一。目前的研究调查了黑海北部海岸的山洪暴发。收集了22次山洪形成的水文、气象、岩性、地貌和人为参数等随机和相对稳定因素的数据。山洪的主要触发因素是该地区的强降雨,但在某些情况下,山洪的发生与几个“非关键”因素的组合有关。发生山洪暴发的流域面积较小(≤351 km2),促使水流迅速集中。极端降水分析表明,21世纪克里米亚半岛河流流域的极端降水呈显著增加趋势,高加索黑海沿岸河流流域的极端降水呈5天最大降水量(r5d)和1天最大降水量(r1d)减少趋势。与此同时,陆地网络数据表明,1961-2020年,阿纳帕和图普塞气象站的r1d呈增加趋势。由于对最长降水范围的统计分析,表明该地区山洪暴发更为频繁。造成重大社会和经济损失的主要原因是黑海沿岸北部洪涝地区人类活动失控。
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引用次数: 0
Simulation of sand and mud transport processes in currents and waves by time-dependent 2DV model 用时变2DV模型模拟水流和波浪中的泥沙输运过程
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-02-01 DOI: 10.1016/j.ijsrc.2024.10.009
Leo van Rijn , Karel Meijer , Kris Dumont , Jan Fordeyn
This paper presents a time-dependent, two-dimensional vertical model for the simulation of sand and mud concentrations, transport and bed level changes in tidal conditions with or without surface waves. The model solves the advection-diffusion equation for suspended sediment. The horizontal velocities and the sediment mixing coefficients are modelled as function of x, z, and t. The settling velocity is constant or modelled as function of the sediment concentration. The sediment mixing coefficient over the water depth is described by flexible expressions based on current and wave parameters which can be modified easily in the input file. To represent mud flocculation and hindered settling processes, the settling velocity can be set as constant or concentration-dependent (input). The bed boundary condition is modelled as a bed concentration as function of the bed-shear stress. The model is valid for low and high sand and mud concentrations including fluid mud concentrations. The numerical SUSTIM2V-model is herein used to simulate sand and mud transport as measured in tidal waters. The model is also successfully used for simulation of high mud concentrations in the near-bed region as measured in the mouth of the Amazon River. The model has also been used to simulate scour along an offshore caisson-type foundation structure.
本文提出了一个随时间变化的二维垂直模型,用于模拟有或没有表面波的潮汐条件下泥沙浓度、输运和床面变化。该模型求解悬浮泥沙的平流扩散方程。水平速度和泥沙混合系数被建模为x、z和t的函数。沉降速度是恒定的或被建模为泥沙浓度的函数。泥沙在水深上的混合系数用基于水流和波浪参数的灵活表达式来描述,并且在输入文件中易于修改。为了表示泥浆絮凝和阻碍沉降过程,沉降速度可以设置为常数或浓度依赖(输入)。将床层边界条件建模为床层浓度作为床层剪切应力的函数。该模型适用于高、低砂泥浓度,包括流体泥浆浓度。本文采用sustim2v数值模型模拟了潮汐水体中实测的泥沙输运。该模型还成功地用于模拟在亚马逊河口测量的近河床区域的高浓度泥浆。该模型还被用于模拟海上沉箱型基础结构的冲刷。
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引用次数: 0
Evaluating the performance of transport equations through long-term records of integrative measured bedload data 通过综合测量的床载数据的长期记录评估输运方程的性能
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-02-01 DOI: 10.1016/j.ijsrc.2024.11.001
Andrea Lammer , Rolf Rindler , Michael Tritthart , Marcel Liedermann , Markus Moser , Dorian Shire-Peterlechner , Sabrina Schwarz , Helmut Habersack
Temporal and spatial variability and a wide range of measured transport rates at comparable flow rates are well-known characteristics of the bedload transport process but represent substantial difficulties in practice and for load calculation. The possibility of measuring the bedload transport process has increased in recent years through the use of technically advanced methods. Since 2011, an integrative bedload monitoring system has been operating on the Urslau River in Austria and has been continuously observing the transport process. This long-term integrative dataset provides the basis for comparing calculation results from commonly used bedload transport formulae with measured data. On the basis of 27 high sediment transport efficiency events, as well as 75 events with reduced sediment availability and 34 events with low sediment availability, this study compares the measured and calculated bedload volumes. In addition, a wide range of measured bedload transport rates are presented for comparable discharges, and values in this range are represented by the formulae shown. The performance of the transport equations is improved by considering measured data from integrative bedload monitoring and by classifying bedload events. The results presented here indicate that, depending on the question considered and by selecting the appropriate formula, it is possible to achieve improved calculation results for practice that are comparable to the measured values.
时间和空间变异性以及在可比流量下测量的大范围输运率是众所周知的河床输运过程的特征,但在实践和负荷计算中却存在很大的困难。近年来,通过使用技术上先进的方法,测量河床输运过程的可能性有所增加。自2011年以来,奥地利乌尔斯劳河上的一个综合河床负荷监测系统一直在运行,并持续观察运输过程。该长期综合数据集为比较常用的层质输运公式的计算结果与实测数据提供了基础。基于27个高输沙效率事件、75个输沙有效度降低事件和34个输沙有效度低事件,比较了实测和计算的床沙体积。此外,对于可比较的流量,给出了一个大范围的测量层质输运率,这个范围内的值用所示公式表示。通过考虑综合床载监测的实测数据和对床载事件进行分类,提高了输运方程的性能。本文给出的结果表明,根据所考虑的问题并通过选择适当的公式,有可能在实践中获得与实测值相当的改进计算结果。
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引用次数: 0
Experimental study on the settling of irregularly shaped sediment particles from the source region of the Yangtze River 长江源区不规则泥沙颗粒沉降试验研究
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-02-01 DOI: 10.1016/j.ijsrc.2024.11.005
Xiaoyong Cheng , Zhijing Li , Yujiao Liu , Zhongwu Jin , Yinjun Zhou , Yisen Wang , Guiqiao Wang , Junfeng Han , Zhixian Cao
Settling plays a pivotal role in sediment transport and morphological evolution of alluvial rivers. Sediment particles in the source regions of large rivers are more likely to feature irregular shapes due to less abrasion than in lower reaches of the rivers. However, the settling of irregularly shaped sediment particles from the source region of a river has to date remained poorly understood. Here, sediment particles were sampled from the Tuotuo River basin in the source region of the Yangtze River. A total of 28 experimental runs were done in a purpose-built settling cylinder to investigate the settling of the sediment particles, with particle Reynolds number, Rep, defined using terminal settling velocity, ranging from 0.22 to 5,939. The results demonstrate that large Rep and irregular particle shape favor unstable settling behavior with wobbling motion and intense velocity fluctuations. An irregular particle experiences larger drag, and, thus, attains a lower terminal velocity than an equivalent sphere, and the shape effect which reduces terminal velocity tends to become significant with increasing Rep and decreasing Corey shape factor. The measured terminal velocities are compared with five empirical formulas. It is shown that the formulas of Dietrich, Haider and Levenspiel, and Wu and Wang are favorable to use (within the range ±20% of the measured data), whereas Zhang's formula and van Rijn's formula may considerably overestimate the terminal velocity, as no shape descriptor is incorporated to account for irregular shape effects. The current study facilitates a new experimental dataset that may be utilized to further investigate sediment settling dynamics. Also, it has direct implications for enhancing the understanding of morpho-dynamics in the source region of the Yangtze River, which may experience significant changes in response to climate change and anthropogenic activities.
沉积在冲积河的输沙和形态演化中起着关键作用。大河源区泥沙颗粒由于较少的磨蚀作用,较下游泥沙颗粒更有可能呈现不规则形状。然而,迄今为止,人们对河流源区不规则形状沉积物颗粒的沉降仍然知之甚少。本文对长江源区沱沱河流域的泥沙颗粒进行了采样。在一个专门建造的沉降筒中,共进行了28次实验,以研究沉积物颗粒的沉降情况,颗粒雷诺数Rep由终端沉降速度定义,范围为0.22至5,939。结果表明,大的Rep和不规则的颗粒形状有利于不稳定沉降行为,具有摆动运动和强烈的速度波动。不规则颗粒受到较大的阻力,因而获得较低的终端速度,并且随着Rep的增大和Corey形状因子的减小,降低终端速度的形状效应趋于显著。实测的终端速度与五个经验公式进行了比较。结果表明,Dietrich、Haider和Levenspiel以及Wu和Wang的公式(在测量数据的±20%范围内)是有利的,而Zhang的公式和van Rijn的公式可能大大高估了终端速度,因为没有纳入形状描述符来考虑不规则形状效应。本研究为进一步研究泥沙沉降动力学提供了新的实验数据集。此外,这对进一步认识长江源区在气候变化和人类活动的影响下可能发生的重大变化具有直接意义。
{"title":"Experimental study on the settling of irregularly shaped sediment particles from the source region of the Yangtze River","authors":"Xiaoyong Cheng ,&nbsp;Zhijing Li ,&nbsp;Yujiao Liu ,&nbsp;Zhongwu Jin ,&nbsp;Yinjun Zhou ,&nbsp;Yisen Wang ,&nbsp;Guiqiao Wang ,&nbsp;Junfeng Han ,&nbsp;Zhixian Cao","doi":"10.1016/j.ijsrc.2024.11.005","DOIUrl":"10.1016/j.ijsrc.2024.11.005","url":null,"abstract":"<div><div>Settling plays a pivotal role in sediment transport and morphological evolution of alluvial rivers. Sediment particles in the source regions of large rivers are more likely to feature irregular shapes due to less abrasion than in lower reaches of the rivers. However, the settling of irregularly shaped sediment particles from the source region of a river has to date remained poorly understood. Here, sediment particles were sampled from the Tuotuo River basin in the source region of the Yangtze River. A total of 28 experimental runs were done in a purpose-built settling cylinder to investigate the settling of the sediment particles, with particle Reynolds number, <span><math><mrow><msub><mtext>Re</mtext><mi>p</mi></msub></mrow></math></span>, defined using terminal settling velocity, ranging from 0.22 to 5,939. The results demonstrate that large <span><math><mrow><msub><mtext>Re</mtext><mi>p</mi></msub></mrow></math></span> and irregular particle shape favor unstable settling behavior with wobbling motion and intense velocity fluctuations. An irregular particle experiences larger drag, and, thus, attains a lower terminal velocity than an equivalent sphere, and the shape effect which reduces terminal velocity tends to become significant with increasing <span><math><mrow><msub><mtext>Re</mtext><mi>p</mi></msub></mrow></math></span> and decreasing Corey shape factor. The measured terminal velocities are compared with five empirical formulas. It is shown that the formulas of Dietrich, Haider and Levenspiel, and Wu and Wang are favorable to use (within the range ±20% of the measured data), whereas Zhang's formula and van Rijn's formula may considerably overestimate the terminal velocity, as no shape descriptor is incorporated to account for irregular shape effects. The current study facilitates a new experimental dataset that may be utilized to further investigate sediment settling dynamics. Also, it has direct implications for enhancing the understanding of morpho-dynamics in the source region of the Yangtze River, which may experience significant changes in response to climate change and anthropogenic activities.</div></div>","PeriodicalId":50290,"journal":{"name":"International Journal of Sediment Research","volume":"40 1","pages":"Pages 62-77"},"PeriodicalIF":3.5,"publicationDate":"2025-02-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143143198","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Chemical composition of sediment and macrozoobenthos of small urban lakes, the Republic of Karelia, Russia 俄罗斯卡累利阿共和国城市小湖泊沉积物和大型底栖动物的化学成分
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-02-01 DOI: 10.1016/j.ijsrc.2024.10.005
Evgeny Savosin , Zakhar Slukovskii
Assessing the benthic communities in water bodies under increasing anthropogenic pressure seems to be an urgent task of scientific research aimed at short-term and long-term monitoring of water bodies. This study focuses on the chemical composition of modern sediment and the current state of macrozoobenthos of small lakes in the Republic of Karelia (Kitaiskoe and Plotichie) influenced by anthropogenic factors. It was discovered that the lakes of Medvezhyegorsk have a higher concentration of heavy metals (such as lead (Pb), cadmium (Cd), molybdenum (Mo), and antimony (Sb)) compared to the Earth’s crust and natural background levels. The current study established the significant impact of industry and transportation on the movement and build up of pollutants in these lakes. The qualitative and quantitative parameters analyzed for the benthic communities in the littoral and profundal zones included the species diversity, the structure of dominant species, and their percentage in the samples. According to the level of macrozoobenthos development, both reservoirs (lakes) were classified as mesotrophic, and according to the values of the chironomid index “K” as moderately polluted. The Pantle–Buck method (saprobic index) showed that the lakes can be classified as polluted (water quality class 4). Macrozoobenthos groups most tolerant to environmental conditions, for example, Chironomidae larvae, prevailed in the studied urban lakes. The economic development of the lakes leads to ecosystem transformation and long-term eutrophication over time affecting the biotic indicators of surface water quality. The results obtained can serve as a basis for complex environmental monitoring of the urbanized territories in the taiga zone.
评估在不断增加的人为压力下的水体中的底栖生物群落似乎是旨在对水体进行短期和长期监测的科学研究的紧迫任务。本文研究了受人为因素影响的卡累利阿共和国(Kitaiskoe和Plotichie)小湖泊现代沉积物的化学成分和大型底栖动物的现状。据发现,梅德维日耶戈尔斯克湖的重金属浓度(如铅(Pb)、镉(Cd)、钼(Mo)和锑(Sb))高于地壳和自然背景水平。目前的研究确定了工业和运输对这些湖泊中污染物的移动和积累的重大影响。分析了滨深带底栖生物群落的物种多样性、优势种结构及其在样品中的比例。根据大型底栖动物的发育程度,两个水库(湖)被划分为中营养型,根据chironomid指数“K”值被划分为中度污染。Pantle-Buck法(污染指数)表明,城市湖泊可被划分为污染湖泊(水质4级)。对环境条件最适应的大型底栖动物类群以手蛾科幼虫为主。随着时间的推移,湖泊的经济发展导致了生态系统的转变和长期的富营养化,影响了地表水水质的生物指标。研究结果可为针叶林城市化地区的复杂环境监测提供依据。
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引用次数: 0
Impacts of grade control structures on riverbed degradation 等级控制结构对河床退化的影响
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-02-01 DOI: 10.1016/j.ijsrc.2024.10.004
Weiming Wu , Ruihua Nie , Kai Wei , Bruce W. Melville , Asaad Y. Shamseldin , Lu Wang
Sediment flux of many rivers has been significantly reduced due to human activities caused by economic development, leading to increasingly severe riverbed degradation. To prevent riverbed degradation, grade control structures (GCSs) have been widely applied in degrading channels. Existing studies have not provided a good understanding of the effects of GCSs on flow characteristics and bed morphology in degrading channels, limiting the management of degrading channels. A series of flume tests with no sediment supply are conducted to investigate the effects of GCSs on upstream water levels and riverbed morphology in degrading channels. The experimental results indicate that: (1) in the initial stage of degradation, the water surface slope in the backwater reach is linearly and negatively correlated with the GCS-height Froude number, based on the average flow velocity upstream of the backwater reach due to GCS and the height of GCS; (2) the effective protection bed length upstream of GCS is approximately equal to the length of the reach where the flow velocity is less than the critical velocity for sediment motion in the backwater zone; (3) for sequential GCSs, the effective protection bed length will decrease if GCS is located in the backwater reach of the downstream GCS. A semi-analytical calculation method of the effective protection length and equilibrium bed profile upstream of GCS in degrading channels is proposed based on the critical condition of sediment motion and weir flow formulas. The computed values by the proposed calculation method agree well with the experimental data of the present study.
由于经济发展引起的人类活动,许多河流的输沙通量显著减少,导致河床退化日益严重。为防止河床退化,坡度控制结构(GCSs)被广泛应用于退化河道。现有研究尚未很好地了解gcs对降解河道流动特性和河床形态的影响,限制了降解河道的管理。在无输沙条件下进行了一系列水槽试验,研究了gcs对退化河道上游水位和河床形态的影响。实验结果表明:(1)在退化初期,基于回水河段上游GCS平均流速和GCS高度,回水河段水面坡度与GCS-高度弗劳德数呈线性负相关;(2) GCS上游有效保护河床长度近似等于回水区流速小于泥沙运动临界流速的河段长度;(3)对于序贯式GCS,如果GCS位于下游GCS的回水河段,则有效保护层长度会减小。基于泥沙运动的临界条件和堰流公式,提出了一种退化河道中GCS上游有效防护长度和平衡河床剖面的半解析计算方法。所提计算方法的计算值与本研究的实验数据吻合较好。
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引用次数: 0
Framework for reservoir sedimentation estimation using the hydrological model and campaign—A case study of A Vuong reservoir in central Vietnam 基于水文模型和运动的水库沉积估算框架——以越南中部阿旺水库为例
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-02-01 DOI: 10.1016/j.ijsrc.2024.11.006
Binh Quang Nguyen , Sameh A. Kantoush , Ngoc Duong Vo , Tetsuya Sumi
Sediment estimation would help practice sustainable watershed management and efficient reservoir operation. Different methods exist to estimate reservoir sedimentation based on the differences in sediment yield flowing in and releasing from the reservoir and successive bathymetric field measurements. This paper investigates the variability in sediment yield from watersheds and sedimentation in the A Vuong reservoir in central Vietnam using the soil and water assessment tool (SWAT) compared with bathymetry mapping. Bathymetry data were collected in 2003, 2015, and 2021 and conducted in 2022. SWAT was calibrated from 1996 to 2008 and validated from 2009 to 2020 using monthly observations. SWAT performs well and can accurately simulate monthly streamflow and sediment yield. The goodness-of-fit analyses suggested that the area list representation of the watershed behavior and satisfactory Sutcliffe efficiency (NSE = 0.86) values for streamflow were obtained during the calibration and validation periods. For sediment simulation, the efficiency is lower than streamflow's, with NSE in the validation values of 0.61. The results showed that the sedimentation estimate from the SWAT model is smaller than that from bathymetry. A Vuong reservoir's annual storage capacity loss due to sedimentation accumulation from the SWAT model and bathymetry was 0.08% and 0.38%, respectively. Based on the bathymetry data, we estimated that the average rate of sedimentation deposition of A Vuong reservoir was 1.3 Mm3/y. The average calculated net deposition value was 4.3 m (0.3 m per year) within fourteen years of operation. The study outcomes demonstrated that the framework approach may transfer to an ungauged catchment and address the complex sedimentation problem in tropical regions.
泥沙估算有助于实现流域可持续管理和水库高效运行。根据水库入沙量和出沙量的差异以及连续的水深野外测量,存在不同的水库沉积估算方法。本文利用土壤和水评价工具(SWAT)与水深测绘相比较,研究了越南中部阿旺水库流域产沙和沉积的变异性。测深数据分别于2003年、2015年和2021年收集,并于2022年进行。SWAT于1996年至2008年进行了校准,并于2009年至2020年进行了月度观测验证。SWAT表现良好,可以准确地模拟月流量和产沙量。拟合优度分析表明,在校准和验证期间,流域行为的面积表表示和流量的Sutcliffe效率(NSE = 0.86)值令人满意。泥沙模拟效率低于径流模拟,NSE在0.61的验证值内。结果表明,SWAT模型估算的沉降量小于测深法估算的沉降量。根据SWAT模型和水深测量结果,Vuong水库因泥沙淤积造成的年库容损失分别为0.08%和0.38%。根据测深资料,估计A Vuong储层的平均沉积速率为1.3 Mm3/y。在14年的运行中,平均计算净沉积值为4.3 m(每年0.3 m)。研究结果表明,框架方法可以转移到未测量的集水区,并解决热带地区复杂的沉积问题。
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引用次数: 0
Interpreting machine learning models based on SHAP values in predicting suspended sediment concentration 基于SHAP值的机器学习模型在悬沙浓度预测中的解释
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-02-01 DOI: 10.1016/j.ijsrc.2024.10.002
Houda Lamane , Latifa Mouhir , Rachid Moussadek , Bouamar Baghdad , Ozgur Kisi , Ali El Bilali
Machine learning (ML) has become a powerful tool for predicting suspended sediment concentration (SSC). Nonetheless, the ability to interpret the physical process is considered the main issue in applying most of ML approaches. In this regard, the current study presents a novel framework involving four standalone ML models (extra trees (ET), random forest (RF), categorical boosting (CatBoost), and extreme gradient boosting (XGBoost)) and their combination with genetic programming (GP). Three metrics (coefficient of correlation (r), root mean square error (RMSE), and Nash–Sutcliffe model-fit efficiency (NSE)) and a more advanced interpretation system SHapley Additive exPlanations (SHAP) are used to assess the performance of these models applied to hydro-climatic datasets for prediction of SSC. The calibration process was based on data from 2016 to 2020, and the validation was done for 2021 data. Further description and application of the framework are provided based on a case study of the Bouregreg watershed. The results revealed that all implemented models are efficient in SSC prediction with NSE, RMSE, and r varying from 0.53 to 0.86, 1.20–2.55 g/L, and 0.83–0.91 g/L respectively. Box plot diagrams confirm the enhanced performance of these combined models, and the best-performing ones for the four hydrological stations being the combined RF + GP model at the Aguibat Ziar station, the combined XGBoost + GP model at the Ain Loudah station, the CatBoost model at the Ras Fathia station, and the RF model at the Sidi Med Cherif station. The interpretability results showed that flow (Q) and seasonality (S) are the features most impacting SSC. These outcomes indicate that the applied models can extract accurate and detailed information from the interactions between the hydroclimatic factors and the generation of sediment by erosion (output). ML approaches illustrated the good reliability and transparency of the models developed for predicting SSC in a semi-arid setting, offered new perspectives for reducing ML models' “black box” character, and provided a useful source of information for assessing the consequences of SSC on water quality. The SHAP system and exploring other interpretable techniques are recommended to provide further information in future research. In addition, incorporating additional input data could enhance SSC predictions and deepen understanding of sediment transport dynamics.
机器学习(ML)已经成为预测悬浮泥沙浓度(SSC)的有力工具。尽管如此,解释物理过程的能力被认为是应用大多数ML方法的主要问题。在这方面,目前的研究提出了一个新的框架,涉及四个独立的机器学习模型(额外树(ET),随机森林(RF),分类增强(CatBoost)和极端梯度增强(XGBoost))及其与遗传规划(GP)的结合。三个指标(相关系数(r)、均方根误差(RMSE)和纳什-萨特克里夫模型拟合效率(NSE))和一个更先进的解释系统SHapley加性解释(SHAP)被用来评估这些模型在水文气候数据集上用于预测SSC的性能。校准过程基于2016年至2020年的数据,并对2021年的数据进行验证。以布雷格流域为例,对该框架进行了进一步的描述和应用。结果表明,所有模型均能有效预测SSC, NSE、RMSE和r分别在0.53 ~ 0.86、1.20 ~ 2.55 g/L和0.83 ~ 0.91 g/L之间。箱形图证实了这些组合模型的增强性能,四个水文站中表现最好的是Aguibat Ziar站的RF + GP组合模型、Ain Loudah站的XGBoost + GP组合模型、Ras Fathia站的CatBoost模型和Sidi Med Cherif站的RF模型。可解释性结果表明,流量(Q)和季节性(S)是影响SSC的主要特征。这些结果表明,应用的模型可以准确、详细地提取水文气候因子与侵蚀产沙(输出)之间的相互作用信息。ML方法说明了在半干旱环境下为预测SSC而开发的模型具有良好的可靠性和透明度,为减少ML模型的“黑箱”特征提供了新的视角,并为评估SSC对水质的影响提供了有用的信息来源。建议使用SHAP系统和探索其他可解释的技术为今后的研究提供进一步的信息。此外,纳入额外的输入数据可以增强SSC预测并加深对沉积物输运动力学的理解。
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引用次数: 0
Inferring sediment deposition trend in data scared wetland impacted by degraded urban catchment 城市集水区退化影响下的数据湿地泥沙沉积趋势推断
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-02-01 DOI: 10.1016/j.ijsrc.2024.10.007
Bhaswatee Baishya, Arup Kumar Sarma
The reduction in water retention capacity due to sedimentation in wetlands poses a serious threat to the ecology of this imperative freshwater resource. This also increases the risk of flooding in the river catchment areas that feed these wetlands. Sediments are mostly produced by unplanned development and hillcutting in upstream catchments. Henceforth, it is crucial to understand the trend in sediment deposition to determine management measures. However, measuring sediment deposition in wetlands is challenging. This study investigates a novel and cost-effective approach to discover trends in sediment deposition within wetlands via geospatial techniques and compares their water extents in the Deepor Beel Wetland, a Ramsar site in Assam, India. The water spread areas were assessed via supervised classified Landsat images and the band rationing technique, i.e., the normalized difference pond index (NDPI). This study establishes that sedimentation causes the water level in wetlands to rise, resulting in an increase in the area of water spread. This often suggests that the lean period water volume is increasing, indicating better health of the stream-wetland ecosystem. However, this apparent increase in water volume is actually due to the displacement of water by the sediment that has been deposited on the bed over time. This approach has identified a reduction in the water holding capacity of the wetland to 9.19 million m3 in 18 years by utilizing geospatially derived water spread and elevation data from two years (2003 and 2021) with comparable rainfall. In the absence of recent and past years with comparable precipitation, the proposed method can still be applied by adjusting the apparent increase in volume by considering the difference in the net inflow volume between the two years of interest. The results of sediment transport toward the wetland, as computed by the Soil and Water Assessment Tool (SWAT) model while accounting for the sediment retention rate of the wetland, strongly agree with the proposed approach. The present approach can be extended to similar stream-wetland ecosystems to examine sediment dynamics and help create better management strategies for wetlands and associated catchment conservation and restoration.
湿地泥沙淤积导致保水能力下降,对这一重要淡水资源的生态构成严重威胁。这也增加了为这些湿地提供水源的河流集水区发生洪水的风险。沉积物主要是由上游集水区的无计划开发和丘陵切割产生的。因此,了解沉积物的沉积趋势对确定管理措施至关重要。然而,测量湿地的沉积物沉积是具有挑战性的。本研究通过地理空间技术探索了一种新颖且经济有效的方法来发现湿地沉积物沉积趋势,并比较了印度阿萨姆邦拉姆萨尔湿地Deepor Beel湿地的水范围。利用监督分类Landsat图像和归一化差池指数(NDPI)波段定量技术对水体扩展面积进行评估。本研究确立了泥沙淤积导致湿地水位上升,导致水体扩散面积增大。这通常表明淡水期水量在增加,表明河流湿地生态系统的健康状况较好。然而,这种明显的水量增加实际上是由于长期沉积在河床上的沉积物取代了水。该方法利用2003年和2021年具有可比降雨量的两年的地理空间水分布和海拔数据,确定了湿地的持水量在18年内减少到919万立方米。在没有最近和过去降水可比较年份的情况下,通过考虑两年之间净流入量的差异来调整表观量的增加,仍然可以应用所提出的方法。在考虑湿地泥沙截留率的情况下,由水土评估工具(SWAT)模型计算的泥沙向湿地输移的结果与所提出的方法非常一致。目前的方法可以扩展到类似的河流-湿地生态系统,以检查沉积物动态,并帮助为湿地和相关的流域保护和恢复制定更好的管理策略。
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引用次数: 0
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International Journal of Sediment Research
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