Water Management Impacts on Don River Annual Runoff under Modern Water Scarcity

IF 0.6 Q4 ECOLOGY
S. V. Dolgov, N. I. Koronkevich, E. A. Kashutina
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引用次数: 0

Abstract

This study investigates the Don River’s behavior from 2014 to 2023, a period marked by exceptionally low annual water flow, with an annual runoff exceedance probability of 80% or greater. Runoff levels dropped considerably compared to the average observed between 1930 and 1980. This decline amounted to 24–29% in the upper basin, and a more substantial reduction of 42–52% occurred in the lower basin. The findings reveal that water scarcity is caused by a combination of climate change and human activities, with the magnitude of water management challenges being a particularly significant contributor. The strain on water management becomes even more significant during periods of low water availability. This is due to the ongoing but unmeasured effects of indirect factors such as changes in irrigation methods and urban expansion, which have been partially compensated for in recent times. We offer a quantitative evaluation of the runoff’s effects, taking into consideration groundwater and surface water withdrawals, water movements in and out of the basin, as well as extra evaporation from the Tsimlyansk Reservoir. Our research demonstrates that the cumulative impact of water management practices substantially contributes to periods of low water flow. Downstream of the Tsimlyansk HPP on the Don River, water flow has decreased by 23–26% compared to the average flow observed between 2014 and 2023. This decline is mainly attributed to the withdrawal and use of surface water, as well as an 11% loss due to evaporation from the Tsimlyansk Reservoir. This research evaluates groundwater extraction impact on runoff losses, differentiating between aquifers that are hydraulically connected to surface water and those that are not. While groundwater extraction and usage within the Don River’s basin contribute to a decrease in its annual water flow, this reduction is relatively minor, estimated at only 2 to 4%. Conversely, the groundwater contribution to river runoff bears a significantly heavier burden, representing 48% of its typical yearly volume.

现代缺水条件下水资源管理对顿河年径流量的影响
本研究调查了2014年至2023年顿河的行为,这一时期的年径流量异常低,年径流量超过80%或更高。与1930年至1980年观测到的平均水平相比,径流水平大幅下降。上盆地下降幅度为24-29%,下盆地下降幅度更大,为42-52%。研究结果表明,水资源短缺是由气候变化和人类活动共同造成的,而水资源管理挑战的规模是一个特别重要的因素。在水资源供应不足的时期,对水资源管理的压力变得更加严重。这是由于灌溉方法的变化和城市扩张等间接因素的持续但无法测量的影响,这些影响在最近得到了部分补偿。我们对径流的影响进行了定量评估,考虑了地下水和地表水的提取,流域内外的水运动,以及茨姆利扬斯克水库的额外蒸发。我们的研究表明,水资源管理实践的累积影响在很大程度上导致了低流量时期。在顿河上的茨姆利扬斯克HPP下游,与2014年至2023年观测到的平均流量相比,水流量减少了23-26%。这种下降主要归因于地表水的提取和使用,以及茨姆利扬斯克水库蒸发造成的11%的损失。这项研究评估了地下水开采对径流损失的影响,区分了与地表水有水力连接的含水层和与地表水没有水力连接的含水层。虽然顿河流域地下水的开采和使用导致了其年水流量的减少,但这种减少相对较小,估计只有2%至4%。相反,地下水对河流径流的贡献承担了更大的负担,占其典型年流量的48%。
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来源期刊
Arid Ecosystems
Arid Ecosystems ECOLOGY-
CiteScore
1.50
自引率
25.00%
发文量
59
期刊介绍: Arid Ecosystems  publishes original scientific research articles on desert and semidesert ecosystems and environment:systematic studies of arid territories: climate changes, water supply of territories, soils as ecological factors of ecosystems state and dynamics in different scales (from local to global);systematic studies of arid ecosystems: composition and structure, diversity, ecology; paleohistory; dynamics under anthropogenic and natural factors impact, including climate changes; studying of bioresources and biodiversity, and development of the mapping methods;arid ecosystems protection: development of the theory and methods of degradation prevention and monitoring; desert ecosystems rehabilitation;problems of desertification: theoretical and practical issues of modern aridization processes under anthropogenic impact and global climate changes.
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