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Evaluating critical hydrodynamic characteristics of rill formation on saturated soil slopes 饱和土质斜坡上细沟形成的临界水动力特性评价
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-08-01 Epub Date: 2025-05-29 DOI: 10.1016/j.ijsrc.2025.05.006
Dandan Li , Xiaoyan Chen , Pingzong Zhu , Wenhao Tan , Tingting Tao , Liwen Ma , Lingyong Kong
As a specific near surface hydrological condition, soil saturation can significantly affect the critical hydrodynamic characteristic and soil erosion rate of rill formation, leading to severe rill erosion. Nevertheless, few studies have investigated the characteristics of critical hydrodynamic parameters and their relationships with rill erosion rate under critical hydrodynamic conditions of rill formation on saturated soil slopes. Consequently, the quantification of critical hydrodynamic parameters and their effects on rill erosion rate under critical hydrodynamic conditions of rill formation on saturated soil slopes is of great significance for understanding the dynamic mechanism of rill formation and evolution and for predicting and controlling soil loss. In this study, indoor simulated rainfall experiments were performed and a new analytical model (Vc(NAM)) was applied to calculate the aforementioned critical parameters under a wide range of hydraulic conditions comprising five slope gradients (SG) (2°, 5°, 10°, 15°, and 20°) and three rainfall intensities (RI) (30, 60, and 90 mm/h). The results indicated that the new analytical model (Vc(NAM)) was suitable for estimating critical hydrodynamic parameters on saturated soil slopes. The critical flow velocity (Vc), the critical shear stress (τc), and the critical stream power (ωc) apparently increased, whereas the critical rill length (Lc) decreased with the increase of slope gradients and rainfall intensities. Moreover, the erosion rate at the critical condition increased with decreasing Lc and increasing Vc, τc, and ωc. Pearson correlation analysis indicated that τc and ωc were significantly positively correlated, whereas Lc was negatively correlated with erosion rate under the critical conditions. Stepwise regression analysis revealed that the erosion rate under critical hydrodynamic conditions of rill formation could be well predicted by τc (R2 = 0.83) with the linear model. The results provide an accurate model for evaluating critical conditions of rill formation and a basis for further understanding the intrinsic dynamic mechanism of rill formation on saturated soil slopes.
土壤饱和作为一种特定的近地表水文条件,会显著影响细沟形成的临界水动力特性和土壤侵蚀速率,导致严重的细沟侵蚀。然而,对于饱和土坡面成沟临界水动力条件下的临界水动力参数特征及其与细沟侵蚀速率的关系研究较少。因此,在饱和土坡面形成细沟的临界水动力条件下,定量研究临界水动力参数及其对细沟侵蚀速率的影响,对于认识细沟形成和演化的动力机制,预测和控制土壤流失具有重要意义。在本研究中,进行了室内模拟降雨实验,并应用了一种新的分析模型(Vc(NAM))来计算上述关键参数,该模型包括5种坡度(SG)(2°、5°、10°、15°和20°)和3种降雨强度(RI)(30、60和90 mm/h)。结果表明,该分析模型(Vc(NAM))适用于饱和土质边坡临界水动力参数的估计。随着坡度和降雨强度的增加,临界流速(Vc)、临界剪应力(τc)和临界水流功率(ωc)明显增大,而临界细沟长度(Lc)减小。临界侵蚀速率随Lc的减小和Vc、τc、ωc的增大而增大。Pearson相关分析表明,临界条件下τc和ωc与侵蚀速率呈显著正相关,Lc与侵蚀速率呈显著负相关。逐步回归分析表明,利用线性模型τc (R2 = 0.83)可以较好地预测细沟地层临界水动力条件下的侵蚀速率。研究结果为评价饱和土边坡上细沟形成的临界条件提供了准确的模型,为进一步认识饱和土边坡上细沟形成的内在动力机制奠定了基础。
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引用次数: 0
Performance of microbially induced calcite precipitation (MICP) as a local scour countermeasure for offshore wind turbine monopile foundation 微生物诱导方解石沉淀(MICP)作为海上风力发电机组单桩基础局部冲刷对策的性能
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-08-01 Epub Date: 2025-05-26 DOI: 10.1016/j.ijsrc.2025.05.003
Zihao Tang , Bruce W. Melville , Naresh Singhal , Asaad Y. Shamseldin , Liang Cheng , Dawei Guan
Microbially induced calcite precipitation (MICP) is an emerging method for mitigating scour and erosion. The present study experimentally investigates the efficacy of MICP as a local scour countermeasure for offshore wind turbine monopile foundations under both clear water and live-bed conditions. Bacteria were enriched using activated sludge. Analyses conducted included urease activity monitoring, unconfined compression testing, and examination using scanning electron microscopy. Various depths for the MICP protection elevation were tested in clear water conditions, and the resulting scour topography was mapped using photogrammetry techniques. Investigations were conducted on bedform migration and leading-edge scour upstream of the MICP protection, considering various protection elevations. The results indicated that MICP protection can provide effective scour protection under both clear water and live-bed conditions. Discussions in this study also extend to the erosion and potential collapse of the MICP protection structure. Flow undercut rate were also examined for evaluating potential failure of MICP protection structures, and the elevation of MICP protection has a significant influence on mitigating flow undercutting. Full protection efficiency was observed under clear water conditions when the MICP protection elevation was at the bed level and the flow intensity was relatively low (V/Vc = 0.65), while the highest average protection efficiency (47.73%) among all flow intensities was recorded when the MICP protection elevation was at 0.6D below the bed.
微生物诱导方解石沉淀(MICP)是一种新兴的减轻冲刷和侵蚀的方法。本研究在清水和活床条件下,实验研究了MICP作为海上风力机单桩基础局部冲刷对策的效果。利用活性污泥富集细菌。分析包括脲酶活性监测、无侧限压缩试验和扫描电镜检查。在清水条件下测试了不同深度的MICP保护标高,并使用摄影测量技术绘制了冲刷地形图。考虑到不同的保护高度,对MICP保护上游的河床迁移和前缘冲刷进行了研究。结果表明,MICP保护层在清水和活床条件下均能提供有效的防冲保护。本研究还讨论了MICP保护结构的侵蚀和潜在崩溃。研究结果表明,MICP保护层的高程对减缓流动下切有显著影响。清水条件下,当MICP防护高程在床面水平且流动强度较低时(V/Vc = 0.65),防护效率最高,平均防护效率为47.73%,当MICP防护高程在床面以下0.6D时。
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引用次数: 0
Prediction of suspended sediment concentration in fluvial flows using novel hybrid deep learning model 基于新型混合深度学习模型的河流悬浮物浓度预测
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-08-01 Epub Date: 2025-03-05 DOI: 10.1016/j.ijsrc.2025.02.004
Sadra Shadkani , Yousef Hemmatzadeh , Amirreza Pak , Soroush Abolfathi
Accurately predicting suspended sediment concentration (SSC) in fluvial systems is essential for environmental monitoring, flood management, and riverine engineering applications. This study introduces a novel hybrid approach for forecasting SSC by leveraging advanced deep learning algorithms. Daily datasets from the U.S. Geological Survey, including discharge (Q) and SSC measurements, were analyzed from 2007 to 2017 at two key locations on the Mississippi River: Chester (CH) and Thebes (TH). The proposed framework integrates feedforward neural networks (FFNN), long short-term memory (LSTM) networks, stochastic gradient descent (SGD), and radial basis function (RBF) models, augmented with a first-order differencing technique. Additionally, hybrid models, including Supervised FFNN-LSTM and Supervised FFNN-SGD, were developed to enhance predictive performance. The dataset was partitioned into training (70%, 2,747 d) and testing (30%, 1,178 d) subsets, with daily temporal resolution. Six input scenarios incorporating lagged parameters were evaluated using performance metrics, including the correlation coefficient (CC), Nash–Sutcliffe efficiency (NSE), scatter index (SI), and Willmott’s index (WI). Sensitivity analysis identified SSCt-1 (i.e., one day before) as the most influential predictor for short-term forecasting. Among the models, the SFFNN-LSTM-6 achieved the highest performance, with CC values of 0.976 for CH and 0.960 for TH, demonstrating the ability to predict SSC effectively even in the absence of current-day discharge data. The proposed hybrid models exhibited exceptional robustness across diverse flow regimes, including extreme environmental conditions, establishing a reliable tool for SSC forecasting in complex fluvial systems.
准确预测河流系统中悬浮泥沙浓度(SSC)对于环境监测、洪水管理和河流工程应用至关重要。本研究介绍了一种利用先进的深度学习算法预测SSC的新型混合方法。美国地质调查局的每日数据集,包括流量(Q)和SSC测量,从2007年到2017年在密西西比河上的两个关键地点:切斯特(CH)和底比斯(TH)进行了分析。该框架集成了前馈神经网络(FFNN)、长短期记忆(LSTM)网络、随机梯度下降(SGD)和径向基函数(RBF)模型,并辅以一阶差分技术。此外,开发了混合模型,包括监督式FFNN-LSTM和监督式FFNN-SGD,以提高预测性能。数据集被划分为训练子集(70%,2,747 d)和测试子集(30%,1,178 d),具有每日时间分辨率。使用相关系数(CC)、Nash-Sutcliffe效率(NSE)、散点指数(SI)和Willmott指数(WI)等性能指标对包含滞后参数的6种输入场景进行了评估。敏感性分析发现SSCt-1(即前一天)是短期预测最具影响力的预测因子。其中,SFFNN-LSTM-6模型表现最好,CH和TH的CC值分别为0.976和0.960,表明即使在没有当日流量数据的情况下也能有效预测SSC。所提出的混合模型在包括极端环境条件在内的各种流动状态下都表现出出色的鲁棒性,为复杂河流系统的SSC预测建立了可靠的工具。
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引用次数: 0
Effects of land management practices on runoff and soil and nutrient losses in the rainfed agroecosystem of the Beles River Basin, Ethiopia 土地管理措施对埃塞俄比亚贝勒斯河流域雨养农业生态系统径流、土壤和养分流失的影响
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-08-01 Epub Date: 2025-03-15 DOI: 10.1016/j.ijsrc.2025.03.002
Yenesew Assaye , Gizaw Desta , Eyayu Molla , Zenebe Adimassu
The Beles River Basin is facing severe soil erosion driven by human-induced activities, leading to significant losses of soil organic carbon (SOC) and nutrients (nitrogen (N) and phosphorus (P)). Effective land management practices (LMPs), including mechanical, biological, and agronomic techniques, are potential strategies for mitigating this degradation, but their effectiveness depends on site-specific and agroecological conditions. However, limited information is available on this aspect of the study area. The objective of the current study was to evaluate the effects of LMPs in the warm subhumid lowlands of the Beles River Basin on runoff, soil loss, and sediment-associated losses of SOC, N, and P from agricultural land. Four LMPs (vetiver grass strips (VGS), conservation agriculture (CA), soil bunds (SB), and fanya juu (FJ)) were evaluated via runoff plots arranged in a randomized complete block design (RCBD) with three replicates. Farmer practices were used as a control (C). The experiments, which were performed over three years (2021–2023), generated runoff, soil loss, and nutrient loss data. The three-year mean annual runoff ranged from 58.5 to 407.5 mm, and the soil loss ranged from 4.3 to 45.4 t/ha, whereas the annual rainfall varied between 1,402 mm in 2021, 1,254 mm in 2022, and 1,261 mm in 2023. On average, runoff was reduced by 36%–85%, and soil loss was reduced by 53%–91% in the LMP-treated plots. Additionally, sediment-associated losses of SOC, N, and P were reduced by 55%–90%, 52%–90%, and 28%–72%, respectively. The results revealed significant differences (p < 0.05) among the treatments in terms of reducing runoff, soil loss, and sediment-associated losses of SOC, N, and P. The mean annual runoff and soil loss rates during the study were 407.5, 230.3, 136.3, 59.6, and 58.5 mm and 45.4, 21.5, 11.1, 4.5, and 4.3 t/ha under the control, VGS, CA, SB, and FJ practices, respectively. The highest rates of runoff and soil loss were observed under the control conditions (407.4 mm and 45.4 t/ha). Runoff, soil loss, SOC, and nutrient (N and P) losses were significantly lower (p < 0.05) in the plots treated with FJ and SB than in the other plots. However, CA and VGS also significantly varied (p < 0.05) in reducing runoff, soil, SOC, and nutrient losses over the years. These results highlight the key role of LMPs in warm subhumid lowland rainfed agroecosystems as effective land management techniques for controlling soil and nutrient loss.
贝勒斯河流域在人为活动的驱动下面临严重的土壤侵蚀,导致土壤有机碳(SOC)和养分(氮(N)和磷(P))大量流失。有效的土地管理实践(LMPs),包括机械、生物和农艺技术,是缓解这种退化的潜在战略,但其有效性取决于具体地点和农业生态条件。然而,关于研究领域的这方面的信息有限。本研究的目的是评估Beles河流域温暖半湿润低地的LMPs对径流、土壤流失以及与农业用地有机碳、氮和磷相关的沉积物损失的影响。采用随机完全区组设计(RCBD)对4种LMPs(香根草条带(VGS)、保护性农业(CA)、土壤带(SB)和凡雅菊(FJ)进行了评价。农民实践作为对照(C)。这些实验进行了三年(2021-2023年),产生了径流、土壤流失和养分流失的数据。年平均径流量在58.5 ~ 407.5 mm之间,土壤流失量在4.3 ~ 45.4 t/ha之间,而年降雨量在2021年1402 mm、2022年1254 mm和2023年1261 mm之间变化。平均而言,在lmp处理的地块上,径流量减少了36%-85%,土壤流失量减少了53%-91%。此外,与沉积物相关的有机碳、氮和磷的损失分别减少了55% ~ 90%、52% ~ 90%和28% ~ 72%。结果显示有显著差异(p <;研究期间,控制、VGS、CA、SB和FJ处理的年径流量和土壤流失率分别为407.5、230.3、136.3、59.6和58.5 mm和45.4、21.5、11.1、4.5和4.3 t/ha。对照条件下的径流量和土壤流失率最高(407.4 mm和45.4 t/ha)。径流、土壤流失、有机碳和养分(N和P)损失显著降低(P <;FJ和SB处理的土壤水分含量显著高于其他处理。然而,CA和VGS也有显著差异(p <;0.05)在减少径流、土壤、有机碳和养分损失方面的作用。这些结果强调了在温暖半湿润低地雨养农业生态系统中,LMPs作为控制土壤和养分流失的有效土地管理技术的关键作用。
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引用次数: 0
Effects of different vegetation litter cover on hydrodynamic characteristics of soil runoff-sediment yield in Taiyi Mountain area of northern China 不同植被凋落物覆盖对太邑山地区土壤流沙产水动力特征的影响
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-08-01 Epub Date: 2025-04-24 DOI: 10.1016/j.ijsrc.2025.04.004
Yuan He , Zihao Fan , Wei Zhao , Zhihao Tian , Dingmeng Hu , Zixu Zhang , Yucun Lu , Peng Gao
Vegetation litter is effective in mitigating surface soil erosion caused by rainfall and runoff. Studying the runoff, sediment yield, and hydrodynamic characteristics of the soil covered by vegetation litter cover is crucial to understanding how vegetation litter cover affects soil erosion. To assess the impacts of different types of vegetation litter on soil erosion in the Taiyi Mountain area of northern China, Quercus acutissima Carruth. (QAC), Pinus densiflora Siebold & Zucc. (PDS), Vitex negundo var. heterophylla Rehd. (VNH), and Themeda japonica Willd. (TJW) litter covered soil were the research subjects, and no-litter covered soil was used as a control check (CK). The process of erosion of soil covered by different vegetation litter under different rainfall intensities (50, 75, and 100 mm/h) with 60 min of rainfall was studied. It was found that compared with CK, the runoff and sediment yield rates of litter-covered soil decreased by 18.95%–44.15% and 21.42%–60.16%, respectively. In terms of the effect on reducing the runoff and sediment yield rate, the performance is QAC > PDS > VNH > TJW. Under varying rainfall intensities, the patterns of runoff and sediment yield fluctuate as rainfall duration increases. Likewise, with the increase in rainfall intensity, the runoff yield rate and sediment yield rate also show an increasing trend. The runoff yield rate was increased by 3.21 and 1.49 times under 100 mm/h compared with 50 and 75 mm/h, respectively. Additionally, there were 16.56 and 1.44 times, respectively, and increases in the sediment yield rate. Hydrodynamically, litter cover increases the Darcy-Weisbach friction coefficient by 1.49–11.15 times, increases the shear stress threshold for initiating soil erosion by about 6.67%–38.01%. This further led to a reduction in the runoff flow velocity and stream power, by approximately 14.87%–67.26% and 7.38%–61.54%, respectively, thereby reducing the degree of soil erosion. The current research demonstrates that the characteristics of soil erosion and sediment yield under vegetation litter cover can be more accurately described by the stream power among the hydrodynamic parameters.
植被凋落物对减轻降雨和径流引起的地表土壤侵蚀是有效的。研究凋落物覆盖土壤的产流、产沙和水动力特征对理解凋落物覆盖对土壤侵蚀的影响至关重要。以太邑山地区不同类型植被凋落物对土壤侵蚀的影响为研究对象。(QAC), Pinus densiflora Siebold &;调查。(PDS),牡荆花变种。(VNH)和Themeda japonica wild。研究对象为凋落物覆盖土壤(TJW),对照对照为无凋落物覆盖土壤(CK)。研究了不同降雨强度(50、75、100 mm/h)和60 min降雨条件下不同植被凋落物覆盖土壤的侵蚀过程。结果表明,与对照相比,凋落物覆盖土壤产流率和产沙率分别降低18.95% ~ 44.15%和21.42% ~ 60.16%。在降低径流产沙率方面,表现为QAC >;PDS祝辞VNH祝辞TJW。在不同降雨强度下,径流产沙模式随降雨持续时间的增加而波动。同样,随着降雨强度的增加,产流率和产沙率也呈增加趋势。与50和75 mm/h相比,100 mm/h下产流率分别提高了3.21倍和1.49倍。产沙速率分别增加了16.56倍和1.44倍。水动力方面,凋落物覆盖使Darcy-Weisbach摩擦系数提高了1.49 ~ 11.15倍,使土壤侵蚀起始剪应力阈值提高了6.67% ~ 38.01%。这进一步导致径流流速降低14.87% ~ 67.26%,河流功率降低7.38% ~ 61.54%,从而降低了土壤侵蚀程度。目前的研究表明,在水动力参数中,水流功率能更准确地描述植被凋落物覆盖下的土壤侵蚀产沙特征。
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引用次数: 0
Probabilistic risk assessment of fifteen metal(loid)s and their mixtures in surface sediment of Hongze Lake (China) using the diffusive gradients in thin films (DGT) technique 利用薄膜扩散梯度(DGT)技术对洪泽湖表层沉积物中15种金属(样物质)及其混合物进行概率风险评估
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-06-01 Epub Date: 2025-02-08 DOI: 10.1016/j.ijsrc.2025.01.007
Changjiang Ma , Yang-Guang Gu , Richard W. Jordan , Shi-Jun Jiang , Meirong Wang
Freshwater lakes in China face increasing environmental pressures due to rapid urbanization and industrialization, with metal pollution emerging as a significant concern. Despite this, the ecological risk assessment of metal mixtures in lake sediment remains limited. The current study addresses this gap by utilizing the diffusive gradients in thin films (DGT) technique to investigate the distribution and ecological risk of metals and arsenic in surface sediment of Hongze Lake, China. Substantial variations in metal concentrations were found across sampling sites, with average values of manganese (Mn) (1,730.56 μg/L) and iron (Fe) (930.58 μg/L) being notably high. The ecological risk quotient (RQ) values for Mn and Fe exceeded 1 at all sites, indicating substantial ecological risks, while copper (Cu) and arsenic (As) had RQ values near or above 1 at most sites. A joint probabilistic risk assessment using the species sensitivity distribution (SSD) method revealed a 30.31% probability of concurrent toxic effects on aquatic organisms. These results highlight the pressing need for proactive measures to mitigate metal contamination risks in Hongze Lake. The current study provides critical insight into the ecological risks associated with metal pollution and underscores the importance of effective environmental management to preserve the lake's ecosystem.
由于城市化和工业化的快速发展,中国淡水湖面临着越来越大的环境压力,金属污染日益成为人们关注的焦点。尽管如此,湖泊沉积物中金属混合物的生态风险评价仍然有限。本研究利用薄膜扩散梯度(DGT)技术研究洪泽湖表层沉积物中金属和砷的分布及其生态风险,解决了这一空白。不同采样点的金属浓度差异较大,其中锰(Mn)的平均值(1730.56 μg/L)和铁(Fe)的平均值(930.58 μg/L)明显偏高。Mn和Fe的生态风险商(RQ)值均超过1,表明存在较大的生态风险,而铜(Cu)和砷(As)的RQ值在1附近或以上。采用物种敏感性分布(SSD)法进行联合概率风险评估,结果显示水生生物并发毒性效应的概率为30.31%。这些结果表明,迫切需要采取积极措施减轻洪泽湖金属污染风险。目前的研究提供了与金属污染相关的生态风险的关键见解,并强调了有效的环境管理对保护湖泊生态系统的重要性。
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引用次数: 0
Evaluation of eco-friendly soil slope stabilization techniques for forest roads by using an Artificial Neural Network (ANN) 基于人工神经网络的森林公路生态土坡稳定技术评价
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-06-01 Epub Date: 2025-02-13 DOI: 10.1016/j.ijsrc.2025.01.011
Kıvanç Yüksel , Neşe Gülci , Abdullah Emin Akay , Sercan Gülci
In this study, the effectiveness of different stabilization techniques implemented on the forest road cut slopes was investigated in terms of controlling erosion and runoff. Wood production residues, hydroseeding, and jute geotextile treatments were applied on study plots located on the example road. The amount of erosion and runoff were measured on the study plots which were established for different slope grades of 20°, 30°, and 40°. Then, the amount of erosion and runoff measured from the plots were compared to determine the performance of stabilization techniques on the cut slope. In the solution process, an Artificial Neural Network (ANN) model, which is one of the machine learning algorithms, was used to predict sediment yield from forest road cut slopes. The sediment yields averaged over the three slope grades from highest to lowest were measured as 6.41, 1.16, 0.65, and 0.45 g/m2 in the control plot with no treatment, jute geotextile, hydroseeding, and wood production residues, respectively. The averaged over the three runoff amounts slope grades from the highest to the lowest were determined as 6.82, 3.71, 1.64, and 1.30 mm/m2 in control the plot, jute geotextile, hydroseeding, and wood production residues, respectively. Comparing to the control plot, wood production residues, hydroseeding, and jute geotextile treatments reduced the sediment yields by 14, 10, and 5 times, respectively. On the other hand, wood production residues, hydroseeding, and jute geotextile applications reduced the runoff amount by 5, 4, and 2 times, respectively. As a result, it was found that wood production residues and hydroseeding treatment can be more efficient in reducing the amount of runoff and sediment yield compared to the jute geotextile treatment. The ANN method achieved high accuracy in predicting sediment yield and it was concluded that the ANN can be used as an effective method to evaluate soil slope stabilization techniques.
本研究从控制侵蚀和径流的角度考察了不同稳定技术在森林道路采伐边坡上实施的有效性。在示例道路上的研究地块上应用了木材生产残留物,加氢播种和黄麻土工布处理。在不同坡度为20°、30°和40°的研究样地上测量了侵蚀量和径流量。然后,比较了从地块测量的侵蚀量和径流量,以确定稳定技术在切坡上的性能。在求解过程中,采用机器学习算法之一的人工神经网络(ANN)模型对森林道路采伐边坡的产沙量进行预测。在未处理、黄麻土工布、加氢播种和木材生产残留物的对照区,从最高到最低三个坡度的平均产沙量分别为6.41、1.16、0.65和0.45 g/m2。三种径流量的坡度等级从高到低分别为6.82、3.71、1.64和1.30 mm/m2,分别用于对照地块、黄麻土工布、加氢播种和木材生产残留物。与对照区相比,木材生产残留物处理、加氢播种处理和黄麻土工布处理的产沙量分别减少了14倍、10倍和5倍。另一方面,木材生产残留物、加氢播种和黄麻土工布的使用分别减少了径流量的5倍、4倍和2倍。结果发现,与黄麻土工布处理相比,木材生产残留物和加氢播种处理可以更有效地减少径流和泥沙产量。人工神经网络在预测产沙量方面取得了较高的精度,可以作为评价土坡稳定技术的有效方法。
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引用次数: 0
Complex morphodynamic processes of a large braided channel in response to different flood flow discharges on the Qinghai-Tibet Plateau 青藏高原大型辫状河道对不同洪水流量的复杂形态动力学响应
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-06-01 Epub Date: 2025-02-11 DOI: 10.1016/j.ijsrc.2025.01.008
Weiqi Ouyang , Zhiwei Li , Hanyou Lu , Yunshuo Cheng , Guo-An Yu , Weiwei Yao , Zhixian Cao
The frequency and intensity of river floods in the Qinghai-Tibet Plateau (QTP) are increasing under the background of climate warming. In particular, the braided channel in the wide valley section in the Source Region of the Yangtze River (SRYR) has undergone drastic adjustments due to recent summer floods and further adjustments are expected in the future as climate change continues. Nonetheless, a lack of a quantitative description of the phenomenon persists. In order to unravel morphodynamic processes of a braided river under different flood flow discharges, a two-dimensional morphodynamic model was established using Delft3D to simulate the local braided channel in the Tuotuo River based on field observations and remote sensing images in the SRYR. The data of 1, 2, 5, and 10-yr flood hydrographs from 1985 to 2020 were obtained, using the hydrological data at the Tuotuohe Gauging Station. Specifically, two groups of actual flood hydrographs were used to simulate the hydrodynamic and riverbed adjustment of the braided channel reach. The following findings were revealed: (i) increases in discharge cause increases of the water level, and thus the flood flow erode and submerge the sandbars. During a flood, the previous branches are replaced by new branches and the braided channel shows a significantly different configuration after the flood. (ii) With the increase of the flood discharge, the amount of sediment erosion and deposition in the braided channels escalates. Specifically, the sediment erosion and deposition of the 10-yr flood will increase by 3.1 times and 4.7 times, respectively, in comparison with the 1-yr flood. (iii) When the discharge is greater than 180 m3/s, the braiding intensity in the wide valley section (>1.2 km) has a significant decreasing trend with the increase in the flood flow. When the discharge is less than 180 m3/s, the correlation between the braiding intensity and flood flow is not significant in the wide reach. (iv) The braiding intensity of the wide reach as flood frequency increases from the 1- to 2-yr events increases by 14.3%, 11.6%, respectively, and decreases for the 5- to 10-yr events by 3.2% and 10.8%, respectively. In the narrow reach, the increases are 25.5% and 11.2%, for the 1- and 2-yr events, respectively, and the decreases are 25.0% and 53.3% for the 5- and 10-yr events, respectively. The parabolic shape of the correlation between the braided intensity and flood discharge increases first, reaches a peak, and then decreases. Overall, the current study contributes to the understanding of the impact of gradually increasing flood discharge on the morphodynamics of braided rivers in the QTP.
在气候变暖的背景下,青藏高原河流洪水发生的频率和强度都在增加。特别是长江源区宽河谷段的辫状河道,由于近期夏季洪水的影响而发生了剧烈的调整,随着气候变化的持续,预计未来还会有进一步的调整。尽管如此,对这一现象仍然缺乏定量的描述。为了揭示不同洪水流量下辫状河的形态动力学过程,基于野外观测和SRYR遥感影像,利用Delft3D软件对沱沱河局部辫状河进行了二维形态动力学模拟。利用沱沱河站的水文资料,获得了1985 ~ 2020年1、2、5、10年的洪水线资料。具体而言,利用两组实际洪水线模拟了辫状河道河段的水动力和河床调整。结果表明:(1)流量的增加引起水位的升高,从而导致洪水侵蚀和淹没沙洲。在洪水发生时,原有的分支被新的分支所取代,在洪水发生后,编织通道的形态发生了明显的变化。(2)随着洪水流量的增加,辫状河道的冲淤量增大。其中,10年洪水的冲沙量和沉积量分别比1年洪水增加了3.1倍和4.7倍。(iii)当流量大于180 m3/s时,宽河谷段(>1.2 km)的编织强度随洪水流量的增加有明显的减小趋势。当流量小于180 m3/s时,宽河段编织强度与洪水流量的相关性不显著。(4)宽河段的编织强度在1 ~ 2年期间随着洪水频率的增加分别增加了14.3%、11.6%,在5 ~ 10年期间分别减少了3.2%、10.8%。在窄范围内,1年和2年的事件分别增加了25.5%和11.2%,5年和10年的事件分别减少了25.0%和53.3%。编织强度与洪流量的相关曲线呈先增大后达到峰值后减小的抛物线形。总体而言,本研究有助于理解逐渐增加的洪水流量对QTP地区辫状河形态动力学的影响。
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引用次数: 0
TOC TOC
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-06-01 Epub Date: 2025-05-10 DOI: 10.1016/S1001-6279(25)00031-9
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引用次数: 0
Simulating fluvial sediment pulses using remote sensing and machine learning: Development of a modeling framework applicable to data rich and scarce regions 利用遥感和机器学习模拟河流沉积物脉冲:开发一种适用于数据丰富和稀缺地区的建模框架
IF 3.5 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2025-06-01 Epub Date: 2025-02-21 DOI: 10.1016/j.ijsrc.2025.02.002
Abhinav Sharma , Celso Castro-Bolinaga , Natalie Nelson , Aaron Mittelstet
Fluvial sediment pulses pose a significant threat to the overall ecological health of river systems. Nonetheless, the scarcity of monitored and published data underscores the importance of devising innovative methods for understanding and measuring how river systems react to the introduction of sediments across the fluvial domain. The objective of this study was to create a modeling framework based on reflectance–turbidity that can be applied in regions with both limited and abundant data. Various combinations of predictor variables, training algorithms including linear regression and additional machine learning methods, and input data availability scenarios were examined to comprehend the factors influencing turbidity prediction on a regional scale. The results indicated that, for Washington state, the random forest algorithm, utilizing a combination of reflectance-based predictors and sediment delivery index (SDI) as predictors, produced the most accurate outcomes (data rich: NSE = 0.54, RSR = 0.68, data scarce: NSE = 0.47, RSR = 0.73). However, when tested on three locations in Washington experiencing sediment pulses, the reflectance–based turbidity prediction model consistently underestimated the peak high and peak low turbidity levels for the Elwha River. The model also exhibited consistent inaccuracies in predicting the initial phase of sediment pulses following the Oso Landslide. Nevertheless, promising results were observed for the Toutle River, downstream to the St. Mt. Helens Volcanic eruption site. Overall, the inclusion of SDI in the model enhanced its efficiency and transferability. By enabling the reconstruction of fluvial sediment pulses in data-scarce regions following dam removals, this integrated approach contributes to advancing our understanding of how rivers respond quantitatively and predictively to these disturbances in sediment supply.
河流沉积物脉动对河流水系的整体生态健康构成重大威胁。尽管如此,监测和公布的数据的缺乏强调了设计创新方法的重要性,以了解和测量河流系统对河流区域引入沉积物的反应。本研究的目的是创建一个基于反射率-浊度的建模框架,该框架可以应用于数据有限和丰富的地区。研究了预测变量、训练算法(包括线性回归和额外的机器学习方法)以及输入数据可用性场景的各种组合,以了解影响区域范围内浊度预测的因素。结果表明,对于华盛顿州,随机森林算法使用基于反射率的预测因子和沉积物输送指数(SDI)作为预测因子的组合产生了最准确的结果(数据丰富:NSE = 0.54, RSR = 0.68,数据稀缺:NSE = 0.47, RSR = 0.73)。然而,当在华盛顿经历沉积物脉冲的三个地点进行测试时,基于反射率的浊度预测模型始终低估了Elwha河的最高和最低浊度水平。该模型在预测Oso滑坡后沉积物脉冲初始阶段时也表现出一贯的不准确性。尽管如此,在St. Mt. Helens火山喷发点下游的图尔特河(Toutle River)观测到了令人鼓舞的结果。总体而言,将SDI纳入模型提高了其效率和可转移性。通过在大坝拆除后数据稀缺的地区重建河流沉积物脉冲,这种综合方法有助于提高我们对河流如何定量和预测地响应这些沉积物供应干扰的理解。
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引用次数: 0
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International Journal of Sediment Research
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