水库沉降管理的稳定性与分岔分析

R. Huffaker, D. Rider, R. Hotchkiss
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引用次数: 2

摘要

世界各地水库的蓄水能力因泥沙淤积而急剧减少,这促使人们转向可持续管理模式。以往的研究考察了各种技术控制水库泥沙的物理能力,并制定了控制水库泥沙最佳可持续利用的经济规则。我们提出了下一个相关的问题:对于特定的技术来说,可持续的油藏管理在结构上是稳定的吗?或者是否存在这样的阈值,即关键管理参数的微小扰动会突然释放出驱动油藏走向灭绝的动力学?过渡型储层的动力特性是什么?我们发现了一个多用途公共水库管理者采用环境友好的“抽水疏浚”沉积物清除技术的特殊情况下的鞍节点分叉。超过分岔阈值,可持续管理突然让位给最终因泥沙淤积而丧失的储存能力。全世界的水库都受到沉积的影响。例如,中国(2)、印度(2)和世界范围内(3)的年储水量估计损失分别为2.3%、0.5%和1%。Batuca和Jordaan(4)对具体的例子进行了分类。这些例子包括俄罗斯苏拉克河上的cirr -lurtsk水库,在7年内沉积了95%;乔治亚州瓦克斯河(Vakhs River)上的古马提水库(Gumati Reservoir), 11年来淤积了90%;库拉河和阿拉木河汇合处的泽莫阿夫查尔水库(俄罗斯)在头两年损失了44%的初始储水量,在接下来的8年里损失了32%,到1967年损失了3.5%。其他的例子包括印度河上的塔贝拉大坝——巴基斯坦同类大坝中最重要的设施——在运行23年后失去了20%的储存能力(5);加州的Matilija大坝,蓄水能力从1947年的7000英亩英尺下降到2005年的不到500英亩英尺(6)。
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Stability and Bifurcation Analysis of Reservoir Sedimentation Management
The alarming loss of water storage capacity to sedimentation in reservoirs worldwide is prompting a paradigm shift toward sustainable management. Previous research has investigated the physical capability of various technologies to control reservoir sediment, and formulated economic rules governing their optimal sustainable use. We ask the next rele- vant questions: Is sustainable reservoir management structurally stable for particular technologies, or do thresholds exist such that small perturbations in key management parameters abruptly unleash dynamics driving the reservoir toward ex- tinction? What are the dynamic properties of reservoirs in transition? We uncover a saddle-node bifurcation for the par- ticular case of a multi-purpose public reservoir manager who adopts the environmentally friendly 'hydrosuction-dredging' sediment removal technology. Beyond the bifurcation threshold, sustainable management abruptly gives way to eventual loss of storage capacity to sedimentation. Reservoirs throughout the world suffer from sedimenta- tion. Examples include estimated annual storage capacity losses of 2.3% in China (2), 0.5% in India (2), and 1% worldwide (3). Specific examples are catalogued by Batuca and Jordaan (4). These include the Cir-lurtsk Reservoir on the Sulak River (Russia) which was 95% sedimented in 7 years; the Gumati Reservoir on the Vakhs River (Georgia) which was 90% sedimented in 11 years; and the Zemo Af- char Reservoir at the confluence of the Kura and Aragi Riv- ers (Russia) which lost 44% of its initial storage capacity in the first 2 years, 32% in the next 8 years, and 3.5% up to 1967. Other examples include the Tarbela Dam on the Indus River—the most important facility of its kind in Pakistan— which lost 20% of its storage capacity after 23 years of op- eration (5); and the Matilija Dam in California whose storage capacity decreased from 7,000 acre feet in 1947 to less than 500 acre feet by 2005 (6).
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