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Exploring best soil conservation practices using the tolerable soil loss limit in central highland of Ethiopia: A case study of Andit Tid watershed 利用埃塞俄比亚中部高地可容忍土壤流失极限探索最佳土壤保持措施:以Andit Tid流域为例
IF 7.3 1区 农林科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2025-01-04 DOI: 10.1016/j.iswcr.2025.01.001
Tilahun Getachew Abebe , Tesfaye Mebrate Lemma , Tesfa Worku Meshesha
Soil erosion is a major issue in Ethiopia, prompting ongoing watershed development campaigns. This study contributes to exploring Best Soil Conservation practices (BSCPs) to reduce erosion rates to/or below Tolerable Soil Loss Limits (TSLLs). To achieve these the study used the SWAT model, coupled with the SWAT Calibration and Uncertainty Procedures (SWAT-CUP), for simulation, sensitivity analysis, calibration, and validation using streamflow and sediment yield data. The calibrated SWAT model was used to assess soil erosion hotspot areas and evaluate the effectiveness of the selected BSCPs: Soil and/or Stone Bund (SSB), Grass strip (GT), reforestation (RF), Soil and/or Stone Bund and grass strip (SSB and GT) and Soil and/or Stone Bund and Reforestation (SSB and RF). The results revealed that 22.9% of the area showed soil loss rates below the TSLL. Furthermore, varying degrees of erosion above the TSLL was observed, with sub-watershed SW-12 experiencing the highest erosion rate (47 t ha−1yr−1) and sub-watershed SW-2 experiencing the lowest (7.8 t ha−1yr−1). Among the evaluated BSCPs, SSB + RF demonstrated the greatest erosion reduction effectiveness at 76.6%, followed by SSB + GT, SSB, RF, and GT, with erosion reduction effectiveness values of 61.7%, 60.0%, 43.3%, and 13.9%, respectively. Based on these findings, SSB + RF is recommended for erosion reduction to or below the TSLL, with implementation priority given to sub-watersheds SW-12, SW-10, SW-3, SW-2, and SW-5, ranked in descending order of erosion rate severity. During implementation, emphasis should be placed on reforestation of plant species of high ecological importance.
土壤侵蚀是埃塞俄比亚的一个主要问题,促使正在进行的流域发展运动。该研究有助于探索最佳土壤保持措施(BSCPs),以将侵蚀率降低到/或低于可容忍土壤流失极限(TSLLs)。为了实现这些目标,该研究使用SWAT模型,结合SWAT校准和不确定度程序(SWAT- cup),利用河流和泥沙产量数据进行模拟、灵敏度分析、校准和验证。利用校正后的SWAT模型对土壤侵蚀热点地区进行评估,并对选定的BSCPs:土壤和/或石滩(SSB)、草带(GT)、再造林(RF)、土壤和/或石滩和草带(SSB和GT)和土壤和/或石滩和再造林(SSB和RF)的有效性进行评估。结果表明,22.9%的区域土壤流失率低于土壤流失率界线。此外,TSLL以上的侵蚀程度也不同,其中小流域SW-12的侵蚀速率最高(47 t ha - 1yr -1),小流域SW-2的侵蚀速率最低(7.8 t ha - 1yr -1)。其中,SSB + RF的减蚀效果最好,为76.6%,其次是SSB + GT、SSB、RF和GT,减蚀效果分别为61.7%、60.0%、43.3%和13.9%。基于这些发现,建议将SSB + RF减少到或低于TSLL,并优先实施SW-12, SW-10, SW-3, SW-2和SW-5子流域,侵蚀速率严重程度由高到低。在实施过程中,重点应放在对生态有重要意义的植物物种的重新造林上。
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引用次数: 0
Prediction and mapping of soil organic carbon in the Bosten Lake oasis based on Sentinel-2 data and environmental variables 基于Sentinel-2数据和环境变量的博斯腾湖绿洲土壤有机碳预测与制图
IF 7.3 1区 农林科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-12-26 DOI: 10.1016/j.iswcr.2024.12.002
Shaotian Li , Xinguo Li , Xiangyu Ge
Soil is the largest carbon pool on the Earth's surface. With the application of remote sensing technology, Soil Organic Carbon (SOC) estimation has become a hot topic in digital soil mapping. However, the heterogeneity of geomorphology can affect the performance of remote sensing in determining soil organic carbon. In the Bosten Lake Watershed in northwestern China, we collected 116 soil samples from farm land, uncultivated land, and woodland. To establish an SOC prediction model, we produced 16 optical remote sensing variables and 9 environmental covariates. Three types of land use were studied: farm land, uncultivated land, and woodland. Five machine learning models were used for these land use types: gradient Tree (ET), Support Vector Machine (SVM), Random Forest (RF), Adaptive gradient Boosting (AdaBoost), and extreme Gradient Boosting (XGBoost). The main driving variables for changes in organic carbon content across the entire sample area were Enhanced Vegetation Index (EVI), Enhanced Vegetation Index 2 (EVI2), Soil-Adjusted Vegetation Index (SAVI); for farm land, it was Clay Index (CI2); for farm land and woodland, it was Color Index (CI). The results showed that in terms of prediction accuracy, RF and XGBoost outperformed SVM. In terms of simulation precision, the ET model's woodland model (R2 = 0.86, RMSE = 7.72), the ET model's farm land model (R2 = 0.82, RMSE = 6.66), and the uncultivated land model of the RF model (R2 = 0.81, RMSE = 1.09) performed best. Compared to global modeling, establishing SOC estimation models based on different land use types yielded more ideal results in this study. These findings provide new insights into high-precision estimation of organic carbon content.
土壤是地球表面最大的碳库。随着遥感技术的应用,土壤有机碳(SOC)估算已成为数字土壤制图中的热点问题。然而,地形的异质性会影响遥感测定土壤有机碳的性能。在中国西北博斯腾湖流域,我们收集了116个土壤样本,包括农田、荒地和林地。利用16个光学遥感变量和9个环境协变量建立土壤有机碳预测模型。研究了三种土地利用类型:农田、荒地和林地。在这些土地利用类型中使用了5种机器学习模型:梯度树(ET)、支持向量机(SVM)、随机森林(RF)、自适应梯度增强(AdaBoost)和极端梯度增强(XGBoost)。整个样区有机碳含量变化的主要驱动变量为增强植被指数(EVI)、增强植被指数2 (EVI2)、土壤调整植被指数(SAVI);农田为粘土指数(CI2);农田和林地为颜色指数(CI)。结果表明,在预测精度方面,RF和XGBoost优于SVM。在模拟精度方面,ET模型的林地模型(R2 = 0.86, RMSE = 7.72)、ET模型的耕地模型(R2 = 0.82, RMSE = 6.66)和RF模型的荒地模型(R2 = 0.81, RMSE = 1.09)表现最好。与全局模型相比,基于不同土地利用类型建立土壤有机碳估算模型的结果更为理想。这些发现为高精度估计有机碳含量提供了新的见解。
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引用次数: 0
Soil erosion elasticity initiative for prioritizing sub-watersheds 优先分流域土壤侵蚀弹性倡议
IF 7.3 1区 农林科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-12-11 DOI: 10.1016/j.iswcr.2024.12.001
Mostafa Zabihi Silabi, Seyed Hamidreza Sadeghi, Mehdi Vafakhah
Quantitative evaluation of soil erosion is necessary to analyze the destructive effects of soil erosion and to identify priority sub-watersheds in different climatic and environmental conditions. The variability of soil erosion thresholds introduced as Erosion elasticity (Ee) can be used to develop reliable management strategies in various temporal and spatial scales. Ee is a potential degree of soil erosion in an area representing the magnitude between maximum and minimum erosion rates. However, the comprehensive prioritization of sub-watersheds according to environmental changes and the concept of Ee is yet to be done. Therefore, the present study introduced the Ee-based approach based on the watershed's maximum and minimum soil erosion capability. The prioritization of the sub-watersheds of the Shazand Watershed of Iran has been exemplified, and the associated results were compared to those of conventional annual soil erosion zoning. Towards that, the mean annual soil erosion and corresponding changes of the study watershed were estimated according to the dynamic changes of vegetation cover and rainfall erosivity. Prioritizing 24-study sub-watersheds was then comparatively conducted using mean annual soil erosion and erosion elasticity approaches. The results of the RUSLE application showed that the soil erosion of the Shazand Watershed varied between 0 and 72 t ha−1 year−1 with a mean annual erosion of 14.35 t ha−1 year−1. The results further revealed that the worst and the best combination of soil erosion factors cause +151% and −62% changes in mean annual soil erosion of the Shazand Watershed. Based on the amount of soil erosion method, sub-watersheds 11, 14, and 23 were placed in the highest priorities, and sub-watersheds 5, 6, 16, and 17 are the lowest priority for management measures. In addition, the results of the Ee approach showed that 28% of the study sub-watersheds were placed in high and relatively high priorities, respectively, and sub-watersheds 9, 13, 18, 19, and 23 stand in the lowest priority. The Ee approach effectively identified the critical sub-watersheds to reduce their tendency to destructive conditions and take appropriate measures to reduce their soil erosion and move them towards ideal conditions. The results can help planners and managers implement the best management measures in priority sub-watersheds, saving time and cost.
定量评价土壤侵蚀是分析土壤侵蚀破坏性效应和确定不同气候环境条件下优先分流域的必要条件。土壤侵蚀阈值的变异性被称为侵蚀弹性(Ee),可用于制定在不同时空尺度上可靠的管理策略。Ee是一个地区潜在的土壤侵蚀程度,表示最大和最小侵蚀率之间的幅度。然而,根据环境变化和Ee概念对流域进行综合优先排序的工作尚未完成。因此,本研究引入了基于流域最大和最小土壤侵蚀能力的e-based方法。举例说明了伊朗沙赞德流域分流域的优先次序,并将相关结果与常规年度土壤侵蚀区划的结果进行了比较。为此,根据植被覆盖度和降雨侵蚀力的动态变化,估算研究流域年平均土壤侵蚀量及其变化。采用年平均土壤侵蚀和侵蚀弹性方法对24个研究子流域进行了优选比较。RUSLE应用结果表明,沙滩流域土壤侵蚀在0 ~ 72 tha−1年−1之间变化,年平均侵蚀量为14.35 tha−1年−1。土壤侵蚀因子最差和最佳组合对沙滩流域年平均土壤侵蚀的影响分别为+151%和- 62%。根据水土流失量法,第11、14、23个子流域的治理措施优先级最高,第5、6、16、17个子流域的治理措施优先级最低。此外,Ee方法的研究结果表明,28%的研究子流域分别被评为高优先级和较高优先级,而第9、13、18、19和23子流域被评为最低优先级。Ee方法有效地识别了关键流域,以减少其破坏性条件的倾向,并采取适当措施减少其土壤侵蚀,使其朝着理想条件发展。研究结果可以帮助规划者和管理者在重点子流域实施最佳管理措施,节省时间和成本。
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引用次数: 0
The effects of armed conflict on natural resources and conservation measures in Tigray, Northern Ethiopia 武装冲突对埃塞俄比亚北部提格雷自然资源和保护措施的影响
IF 7.3 1区 农林科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-11-29 DOI: 10.1016/j.iswcr.2024.11.004
Hailemariam Meaza , Tesfaalem Ghebreyohannes , Zbelo Tesfamariam , Girmay Gebresamuel , Biadgilgn Demissie , Dawit Gebregziabher , Jan Nyssen
A heavy armed conflict erupted in Tigray region of Ethiopia in 2020, and the crisis continued up to 2022. This study investigates the impacts of this crisis on the status of natural resources, and Soil and Water Conservation (SWC) efforts. We collected primary data through field observations, measurements, interviews and group discussions during the wartime. We also reviewed published articles and official archives to complement the primary data, which were often challenging to obtain due to the war. We found that vegetated landscapes were damaged by artillery fire and bombings. The average depth of the surveyed bomb craters along the asphalts was 1.15 ± 0.47 m (n = 16), whereas the average surface diameter of the craters and their rim was 2.66± 0.67 m. In addition, the construction of numerous military trenches along croplands and hillsides exposed the soil particles into erosion and water pollution. The conflict also halted SWC efforts on various land uses, which were carried out annually during peacetime. For instance, 20,591 km/year of stone bunds were not constructed per year due to the crisis. Moreover, terraces and stone bunds were demolished to construct temporary ground fortifications. Indirectly, the critical energy crisis further increased pressure on forests. In this context, the poor farmers shift their livelihood strategies from the long-term sustainability to immediate economic recovery during the critical time. To conclude, the pathways of the warfare undermined the status of natural resources, and the ongoing decades of re-greening programs. Therefore, our ground-based findings can be used to prioritize and rehabilitate the war-damaged landscape services.
2020年,埃塞俄比亚提格雷地区爆发严重武装冲突,危机一直持续到2022年。本研究调查了这一危机对自然资源状况和水土保持(SWC)工作的影响。我们在战时通过实地观察、测量、访谈和小组讨论收集了第一手资料。我们还审查了已发表的文章和官方档案,以补充由于战争而往往难以获得的原始数据。我们发现植被被炮火和轰炸破坏了。所测弹坑沿沥青路面的平均深度为1.15±0.47 m (n = 16),弹坑及其边缘的平均表面直径为2.66±0.67 m。此外,沿着农田和山坡修建的大量军事壕沟暴露了土壤颗粒,使其受到侵蚀和水污染。冲突也停止了在和平时期每年进行的各种土地使用的SWC努力。例如,由于危机,每年没有建造20,591公里的石带。此外,梯田和石埂被拆除,以建造临时的地面防御工事。严重的能源危机间接地进一步增加了对森林的压力。在此背景下,贫困农民在关键时期将生计战略从长期可持续性转向立即恢复经济。总之,战争的路径破坏了自然资源的地位,也破坏了持续数十年的重新绿化计划。因此,我们基于地面的研究结果可以用于优先考虑和恢复战争破坏的景观服务。
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引用次数: 0
Impacts of topography on the morphological indices of ephemeral gullies in the Chinese mollisol region 地形对中国软土层地区短命沟形态指标的影响
IF 7.3 1区 农林科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-11-22 DOI: 10.1016/j.iswcr.2024.11.003
Luyou Zhao , Fenli Zheng , Ting Zhao , Ximeng Xu , Xuesong Wang , Hongqiang Shi , Lun Wang , Binglong Wu
Ephemeral Gully (EG) erosion is a main erosion type on sloping croplands in the Chinese Mollisol region, causing severe land degradation and crop yield reduction, but how topographic factors, such as slope gradient, slope aspect, and upslope and lateral drainage areas, affect the morphological indices of EGs is still unclear. Thus, this study applied a high-resolution 5-cm Digital Elevation Model (DEM) obtained from Unmanned Aerial Vehicles (UAV) aerial surveys to quantify the impacts of topography on the morphological indices of EGs in a typical Mollisol region located in Keshan County, Heilongjiang Province. The results showed that the length of EGs decreased with an increase in slope gradient or increased with an increase in upslope and lateral drainage areas. The distribution density, dissected degree, and vertical gradient of EGs increased with an increase in slope gradient or a decrease in the upslope and lateral drainage areas. Moreover, 10 ha and 5 ha areas were critical values regarding the impacts of the upslope drainage area and lateral drainage area on the width, depth, and volume of EGs, respectively, and 0.11 m m−1 and 0.03 m m−1 were critical values regarding the impacts of slope gradients of the upslope drainage area and lateral drainage area on the width, depth, and volume of EGs, respectively. In addition, the number of EGs on sunny and semi-sunny slopes was 1.8 times higher than that on shady and semi-shady slopes. In particular, the topographic thresholds of EG occurrence, synthesizing upslope and lateral gradients, and upslope and lateral drainage areas, were determined, overcoming the current research deficiency of considering only the upslope drainage area and ignoring the lateral drainage area. The results provide an important basis for understanding EG erosion development and implementing precise soil conservation measures.
短期沟壑侵蚀是中国Mollisol地区坡耕地的主要侵蚀类型,造成严重的土地退化和作物减产,但坡度、坡向、上、侧向流域等地形因素对短期沟壑侵蚀形态指标的影响尚不清楚。因此,本研究利用无人机(UAV)航测获得的高分辨率5厘米数字高程模型(DEM),量化了地形对黑龙江省克山县典型Mollisol地区EGs形态指标的影响。结果表明:随着坡面坡度的增大,坡面长度减小,随着坡面和侧向排水面积的增大,坡面长度增大;EGs分布密度、解剖程度和垂直梯度随坡度的增大而增大,在上坡和侧向排水区呈减小趋势。10 ha和5 ha面积分别是上坡流域和侧坡流域对EGs宽度、深度和体积影响的临界值,0.11 m m−1和0.03 m m−1分别是上坡流域和侧坡流域坡度对EGs宽度、深度和体积影响的临界值。阳坡和半阳坡上的茄子数量是阴坡和半阴坡上茄子数量的1.8倍。特别是综合上坡和侧向坡度、上坡和侧向流域,确定了EG发生的地形阈值,克服了目前研究中只考虑上坡流域而忽略侧向流域的不足。研究结果为了解土壤侵蚀的发展规律和实施精准的水土保持措施提供了重要依据。
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引用次数: 0
The potential of runoff retention structures as a strategy to control urban gullying in tropical cities 径流截留结构作为控制热带城市沟壑区策略的潜力
IF 7.3 1区 农林科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-11-13 DOI: 10.1016/j.iswcr.2024.11.002
Eric Lutete Landu , Guy Ilombe Mawe , Fils Makanzu Imwangana , Charles Bielders , Olivier Dewitte , Jean Poesen , Aurélia Hubert , Matthias Vanmaercke
Rapid and chaotic urbanization leads to the formation of urban gullies in many tropical cities of the Global South. To prevent and limit the destructive impacts of these gullies, runoff retention structures are often constructed. Yet, earlier research indicates that these measures are largely ineffective in reducing urban gully expansion. This study aims to understand why. We conducted detailed field surveys in two representative catchments affected by urban gullies in Kinshasa (Democratic Republic of the Congo) and characterized all existing runoff retention structures. We then used the Soil Water Management Model (SWMM) to evaluate the likely influence of these structures on runoff volumes and peak discharges. Although most parcels (77%–88%) in the catchments have at least one runoff retention structure, their overall effect catchment runoff is limited (e.g., only 25–30% reduction of the total runoff volume for an event with a return period of 2 years). One key reason is that many structures are too small and poorly maintained, reducing their already limited storage capacities. Additionally, they are typically unequally distributed within the catchments (with fewer measures upstream) and not proportional to the parcel size, leading to some oversized and many undersized structures. Overall, we demonstrate that, while current efforts are largely ineffective, coordinated implementations of runoff retention structures proportional to parcel size offer promising perspectives for better controlling urban gully erosion.
在全球南方的许多热带城市,快速而混乱的城市化导致了城市沟壑的形成。为了防止和限制这些沟渠的破坏性影响,经常建造径流截流结构。然而,早期的研究表明,这些措施在减少城市沟壑扩张方面基本上是无效的。本研究旨在了解其中的原因。我们在金沙萨(刚果民主共和国)两个受城市沟渠影响的代表性集水区进行了详细的实地调查,并对所有现有的径流保留结构进行了表征。然后,我们使用土壤水管理模型(SWMM)来评估这些结构对径流量和峰值流量的可能影响。虽然汇水区的大多数地块(77%-88%)至少有一个径流保留结构,但它们对汇水区径流的总体影响是有限的(例如,在一个2年的回收期中,仅减少总径流量的25-30%)。一个关键原因是许多结构太小,维护不善,减少了它们本就有限的存储容量。此外,它们通常在集水区内分布不均(上游测量较少),与地块大小不成比例,导致一些过大和许多较小的结构。总的来说,我们证明,虽然目前的努力在很大程度上是无效的,但与地块大小成比例的径流保留结构的协调实施为更好地控制城市沟壑侵蚀提供了有希望的前景。
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引用次数: 0
Environmental assessment based on soil loss, deforestation in permanent preservation areas, and water quality applied in the Itacaiúnas Watershed, Eastern Amazon 基于土壤流失、永久保护区森林砍伐和亚马逊东部Itacaiúnas流域水质的环境评估
IF 7.3 1区 农林科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-11-06 DOI: 10.1016/j.iswcr.2024.11.001
Paulo Rógenes Monteiro Pontes, Rosane Barbosa Lopes Cavalcante, Gabriel Negreiros Salomão, José Tasso Felix Guimarães, Roberto Dall’Agnol
To understand how various environmental pressures may threaten the Amazon territory, specifically its hydrographic basins, it is crucial to guide key management actions such as soil conservation, environmental preservation, and forest restoration. This paper, based on a detailed study conducted in the Itacaiúnas River Watershed (IRW) located in the Carajás mining province—one of the most significant metallogenetic provinces globally and within the Arc of Deforestation in the Amazon—proposes a new index to assess environmental threats or vulnerabilities. The index evaluates soil loss, deforestation in permanent preservation areas, and water quality—key environmental issues in watershed management. Using geoprocessing and remote sensing techniques, we applied the index across the entire catchment area and at the beginning of the drainage network (a proxy for river springs). Our findings reveal that: i) 68% of unit catchments (32% of headwaters) exhibit “High” or “Very High” soil loss vulnerability; ii) 69% of unit catchments (32% of headwaters) have more than 20% of their permanent preservation areas deforested, representing the primary threat among the three criteria to the basin; iii) Only 4.7% of unit catchments (2% of headwaters) present any chemical risk related to water consumption. The combined criteria (simple arithmetic mean of normalized values) indicate that the east-central and southern parts of the watershed have higher index values, necessitating greater attention to soil conservation. In contrast, the center-western area of the basin, characterized by conservation units and indigenous land, showed low index values but remains at risk primarily due to soil loss if environmental preservation actions are not maintained.
要了解各种环境压力如何威胁亚马逊地区,特别是其水文盆地,至关重要的是要指导关键的管理行动,如土壤保持、环境保护和森林恢复。本文基于对位于Carajás矿业省(全球最重要的成矿省之一)的Itacaiúnas河流流域(IRW)进行的详细研究,提出了一个评估环境威胁或脆弱性的新指标。该指数评估了土壤流失、永久保护区的森林砍伐和水质——流域管理中的关键环境问题。利用地理处理和遥感技术,我们将该指数应用于整个集水区和排水网络的开始(河流泉的代理)。我们的研究结果表明:1)68%的单位集水区(32%的水源)表现出“高”或“非常高”的土壤流失脆弱性;Ii) 69%的单位集水区(32%的水源)有超过20%的永久保护区被砍伐,在三个标准中对流域构成主要威胁;只有4.7%的单位集水区(2%的水源)存在与用水有关的化学品风险。综合指标(归一化值的简单算术平均值)表明,流域中东部和南部的指数值较高,需要加大对土壤保持的重视。相比之下,以保护单元和土著土地为特征的盆地中西部地区指数较低,但如果不采取环境保护行动,则主要由于土壤流失而仍然存在风险。
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引用次数: 0
Exploring soil erosion and reservoir sedimentation through the RUSLE model and bathymetric survey 通过RUSLE模型和水深测量探索土壤侵蚀和水库沉积
IF 7.3 1区 农林科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-22 DOI: 10.1016/j.iswcr.2024.10.005
Constantin Nistor , Ionuț Săvulescu , Gabriela Ioana-Toroimac , Sorin Carablaisă
The aim of the paper was to compare the soil erosion in a river catchment with the sediment volume accumulated at the river mouth. Firstly, the sediment yield was estimated in GIS based on the soil loss according to the RUSLE model, and then further integrated into the sediment production equation. Following this, we estimated the sediment volume accumulated at the river mouth based on the diachronic overlap of topographic and bathymetric data. This methodology was validated for the Eselnita catchment exiting into the Iron Gates I Reservoir. The LS factor has an average value of 4, with lower values for the forest cover. The C factor has an average value of 0.057 being statistically correlated with the RUSLE result. The average soil loss was estimated at approximately 1.89 t ha−1 yr −1, a value that is validated by previous studies as a low risk of erosion at national scale. The sediment transfer model indicates a distribution of cells sediment production strongly correlated with the time travel to the discharge channels. Overall, the sediment volume obtained by using the RUSLE model corresponds to about 70% of the sediment volume accumulated at the river mouth during 53 years (1970–2022). The difference in sedimentation may be due to human activities along the river mouth's banks to extend the built-up area and to enjoy the waterscape. This paper is relevant for the topic of reservoir sedimentation and recommends the use of the RUSLE model to predict the sediment contribution, especially for small ungauged catchments.
本文的目的是比较河流流域的土壤侵蚀与河口的泥沙蓄积量。首先,根据RUSLE模型在GIS中基于土壤流失量估算出产沙量,然后将产沙量进一步整合到产沙方程中。在此基础上,基于地形和水深资料的历时重叠,估算了河口沉积量。该方法在Eselnita集水区进入铁门1号水库的情况下得到了验证。LS因子的平均值为4,森林覆盖的LS因子值较低。C因子均值为0.057,与RUSLE结果有统计学相关性。据估计,平均土壤流失量约为1.89吨/公顷- 1年- 1年,这一数值已被先前的研究证实为全国范围内的低侵蚀风险。泥沙输运模型表明,细胞产沙量的分布与排水渠的时间旅行密切相关。总体而言,RUSLE模型得到的沙体积相当于53 a(1970-2022)河口累积沙体积的70%左右。沉积物的差异可能是由于人类在河口沿岸的活动,以扩大建成区和享受水景。本文与水库沉积有关,并建议使用RUSLE模型来预测泥沙贡献,特别是对于未测量的小集水区。
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引用次数: 0
Establishing and verifying soil quality index model based on GIS and remote sensing for cultivated lands under semi-humid terrestrial ecosystem 基于GIS和遥感的半湿润陆地生态系统耕地土壤质量指数模型的建立与验证
IF 7.3 1区 农林科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-17 DOI: 10.1016/j.iswcr.2024.10.004
Ismail Fatih Ormanci , Orhan Dengiz
Sustainable and efficient use of agricultural land depends on the potential characteristics of the soil. This potential directly affects the phenological growth and development of the crop to be grown. For these reasons, soil quality studies are of great importance in determining the products to be grown and the sustainability of the agriculture to be carried out. In this study, carried out in the Engiz Basin, a semi-humid terrestrial ecosystem of the Black Sea region, 250 soil samples were sampled from agricultural areas throughout the basin and a total of 26 soil physical, chemical and biological criteria were measured. Using Geographic Information Systems, Remote Sensing, Fuzzy-Analytical Hierarchy Process and Standard Scoring Function, soil quality models were constructed according to the obtained soil criteria. In addition, principal component analysis was used to select a minimum data set of the most sensitive indicators. The main physical criterion has the highest weight value with 0.611. The weight values for the highest sub-criteria of each main criterion - physical, chemical, biological, and fertility - were determined as slope (0.226), organic matter (0.425), microbial biomass carbon (0.512), and nitrogen (0.245), respectively. Geostatistical models were also used to produce maps of the spatial distribution of soil quality index values for the study area. Moreover, satellite image analysis and field studies (such as; data was collected from a face-to-face survey conducted with 51 farmers) were carried out to verify the obtained SQI distribution maps. The highest r2 values of 0.9004 were found between the SQITDS-L model and NDVI biomass reflectance values. Furthermore, when analyzing the statistical relationship between soil quality classes and yield and economic values obtained from the field, the high r2 value (0.8209) was determined.
农业用地的可持续和有效利用取决于土壤的潜在特性。这种潜力直接影响到作物的物候生长和发育。由于这些原因,土壤质量研究对于确定要种植的产品和要进行的农业的可持续性非常重要。本研究在黑海地区半湿润陆地生态系统Engiz盆地进行,从整个盆地的农业区采集了250个土壤样本,共测量了26个土壤物理、化学和生物指标。利用地理信息系统、遥感、模糊层次分析法和标准评分函数,根据得到的土壤标准构建土壤质量模型。此外,采用主成分分析方法选取最敏感指标的最小数据集。主物理指标的权重值最高,为0.611。各主要标准(物理、化学、生物和肥力)中最高子标准的权重值分别为坡度(0.226)、有机质(0.425)、微生物生物量碳(0.512)和氮(0.245)。地质统计模型还用于绘制研究区域土壤质量指标值的空间分布图。此外,卫星图像分析和实地研究(例如;数据收集自对51名农民进行的面对面调查),以验证获得的SQI分布图。SQITDS-L模型与NDVI生物量反射率的r2值最高,为0.9004。进一步分析土壤质量等级与田间产量和经济价值的统计关系,得到r2高值(0.8209)。
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引用次数: 0
Non-consistent changes and drivers of water-sediment fluxes in the yarlung tsangpo river basin of the Tibetan plateau 青藏高原雅鲁藏布江流域水沙通量的非一致变化及其驱动因素
IF 7.3 1区 农林科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-17 DOI: 10.1016/j.iswcr.2024.10.003
Dongmei Zhao , Donghong Xiong , Kunlong He , Baojun Zhang , Fan Zhang , Han Wu , Haiyan Fang , Wenduo Zhang , Changyan Zhou , Xiaodan Wang
Variations in water-sediment fluxes and their driving mechanisms are critical to riverine ecosystems and management. Yet, current estimates of the response of water and sediment flux remain insufficiently quantified, limited by the scarcity of long-term hydrological records in the alpine regions. Here, we leverage decadal observations in the Yarlung Tsangpo River basin, to investigate the dynamic shifts in water-sediment fluxes from 1955 to 2020 and elucidate their linkage to a warming and wetting climate, snowmelt, and environmental greening (including natural- and human-induced greening) in the different spatial and temporal scale. Major drivers of shifts in water-sediment flux are identified by using wavelet coherence and variance partitioning of redundancy analysis. The results highlight that observational data from four gauging stations (i.e., Lhaze, Nugesha, Yangcun, and Nuxia) uncover a substantial decrease in Suspended Sediment Load (SSL) (Nuxia: 12.302 × 104 t/yr, P < 0.05) in the downstream with consistently increasing runoff and precipitation. Especially during the flood season (July to September), the dam/reservoir construction caused a median decrease in SSL. Dropping sediment offsets the slightly rising SSLs in the midstream and upstream (upper Yangcun: 14.8 × 104 t/yr, P > 0.05). Up to 80% of sediment was sourced from the middle stretch between Lhaze and Nugesha despite it supplied with lower regional runoff generation. Nevertheless, the downstream zone experienced the transition from a sediment source to a deposition area around 1998. We further found the negative and positive effects between water-sediment fluxes and revegetation, and demonstrated that employing NDVI to evaluate human-induced vegetation greening might overestimate the impact of ecological restoration programs on water-sediment fluxes. Attribution analysis indicates that precipitation was not the primary contributor to runoff and SSL changes in all stretches of the basin. In the upstream, temperature and associated snowmelt can be more important than precipitation. Compared to before 1998, precipitation is still the primary driver of change in downstream runoff change after 1998, whilst vegetation restoration, rather than precipitation, dominates the reduction in downstream SSL. These findings have far-reaching significance for watershed managers and decision-makers in terms of developing effective strategies for water resources and soil erosion control.
水沙通量的变化及其驱动机制对河流生态系统和管理至关重要。然而,由于高山地区长期水文记录的缺乏,目前对水和沉积物通量响应的估计仍然不够量化。本文利用雅鲁藏布江流域的年代际观测资料,研究了1955 - 2020年雅鲁藏布江流域水沙通量的动态变化,并在不同时空尺度上阐明了其与气候增湿、融雪和环境绿化(包括自然和人为绿化)的联系。利用小波相干性和方差分割的冗余分析方法,确定了水沙通量变化的主要驱动因素。结果表明,拉泽、女格沙、阳村和女霞4个台站的观测数据显示,悬沙荷载(SSL)明显减少(女霞:12.302 × 104 t/yr, P <;0.05),径流和降水持续增加。特别是在汛期(7 ~ 9月),大坝/水库的建设导致了溢流的中值下降。沉积物的下降抵消了中上游略微上升的SSLs(阳村上游:14.8 × 104 t/yr, P >;0.05)。高达80%的泥沙来自拉扎兹和努格沙之间的中间地带,尽管它提供了较低的区域产流。然而,1998年前后,下游地区经历了从沉积源到沉积区的转变。研究还发现了水沙通量与植被恢复之间的正、负作用,并表明采用NDVI评价人为植被绿化可能高估了生态恢复项目对水沙通量的影响。归因分析表明,降水并不是流域各伸展段径流和SSL变化的主要贡献者。在上游,温度和相关的融雪可能比降水更重要。与1998年以前相比,1998年以后降水仍然是下游径流变化的主要驱动因素,而植被恢复而不是降水主导了下游径流变化的减少。这些发现对流域管理者和决策者制定有效的水资源和土壤侵蚀控制策略具有深远的意义。
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International Soil and Water Conservation Research
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