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首页> 外文期刊>Philosophical Transactions of the Royal Society of London, Series B. Biological Sciences >The role of extreme events in the impacts of selective tropical forestry on erosion during harvesting and recovery phases at Danum Valley, Sabah
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The role of extreme events in the impacts of selective tropical forestry on erosion during harvesting and recovery phases at Danum Valley, Sabah

机译:极端事件在沙巴州达努姆山谷收获和恢复阶段的选择性热带森林对侵蚀的影响中的作用

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摘要

Ten years' hydrological investigations at Danum have provided strong evidence of the effects of extremes of drought, as in the April 1992 E1 Nino southern oscillation event, and flood, as in January 1996. The 1.5 km~2 undisturbed forest control catchment experienced a complete drying out of the stream for the whole 1.5 km of defined channel above the gauging station in 1992, but concentrated surface flow along every declivity from within a few metres of the catchment divide after the exceptional rains of 19 January 1996. Under these natural conditions, erosion is episodic. Sediment is discharged in pulses caused by storm events, collapse of debris dams and occasional landslips. Disturbance by logging accentuates this irregular regime. In the first few months following disturbance, a wave of sediment is moved by each storm, but over subsequent years, rare events scour sediment from bare areas, gullies and channel deposits. The spatial distribution of sediment sources changes with time after logging, as bare areas on slopes are revegetated and small gullies are filled with debris. Extreme storm events, as in January 1996, cause logging roads to collapse, with landslides leading to surges of sediment into channels, reactivating the pulsed sediment delivery by every storm that happened immediately after logging. These effects are not dampened out with increasing catchment scale. Even the 721 km~2 Sungai Segama has a sediment yield regime dominated by extreme events, the sediment yield in that single day on 19 January 1996 exceeding the annual sediment load in several previous years. In a large disturbed catchment, such road failures and logging-activity-induced mass movements increase the mud and silt in floodwaters affecting settlements downstream. Management systems require long-term sediment reduction strategies. This implies careful road design and good water movement regulation and erosion control throughout the logging process.
机译:在达努姆(Danum)进行的十年水文调查提供了强有力的证据,证明极端干旱的影响(如1992年4月的E1尼诺南部振荡事件)和洪水(如1996年1月的影响)。1.5km〜2的未扰动森林控制流域经历了完全在1992年,测量站上方整个1.5 km的确定河道干the了河水,但在1996年1月19日的异常降雨之后,在集水区的几米范围内沿每个偏角集中了地表水。在这些自然条件下,侵蚀是偶发的。沉积物以暴风雨,碎石坝倒塌和偶尔的山崩引起的脉动释放。伐木造成的干扰加剧了这种不规则状况。扰动后的最初几个月,每次风暴都会产生一波沉积物,但是在随后的几年中,罕见事件冲刷了裸露区域,沟渠和河道沉积物中的沉积物。伐木后,沉积物源的空间分布随时间而变化,因为斜坡上的裸露区域被重新植被,小沟渠中充满了碎屑。像1996年1月那样的极端风暴事件导致伐木公路倒塌,滑坡导致泥沙涌入河道,每次伐木后立即发生的暴风雨都会重新启动脉冲式泥沙输送。随着集水规模的增加,这些影响不会减弱。甚至在721 km〜2 Sungai Segama的沉积物产量体系中,极端事件也占主导地位,1996年1月19日的那一天的沉积物产量超过了前几年的年度沉积物负荷。在一个受干扰的大流域,这种道路故障和伐木活动引起的群众运动增加了洪水中的泥沙和淤泥,影响了下游的定居点。管理系统需要长期减少沉积物的策略。这意味着在整个测井过程中要进行仔细的道路设计,良好的水流调节和侵蚀控制。

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