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Morphometry of Selected Watersheds, their Bed Sediment Load Characteristics and Reclamation Measures for Sediment Control in Outer Himalayas

机译:选定流域的形态学,沉积物荷载作用及沉积物控制中的沉积物载荷特性及沉积物控制

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The Himalayas cover an area of about 50 m ha and there has been a very rapid increase in the developmental activities. A near experimental population growth has placed a further heavy demand on already limited natural resources. Debris load production from stream banks, land slides and mine waste causes in-equilibrium in stream flow regimes and further cause extensive damage to life and property. The paper deals with-(a) determination of Characteristics of Watershed situated in Himalayas and Shiwaliks, (b) to establish relationships between channel morphological parameters with drainage area and channel length upstream, (c) to evaluate the performance of the management strategies in the reduction of runoff and debris load production rates. The studies conducted clearly established that - a) bed material size increased up to about one-fourth to one-third of the length of torrent and decreased thereafter. Such a behavior is due to both colluvial and gravitational forces. b) an inverse relationship exist between channel width and local bed slope, c) the reclamation measures reduced runoff from almost 55 % to 33 % and debris load from 550 tonnes/ha/year to 8.0 tonnes/ha. When conservation measures are well planned and implemented scientifically would not only reduce runoff and debris load but also improve dry weather flow and sustain for a longer period. The conservation measures when implemented in a watershed situated in Himalayas proved effective in attenuating the peak rates of runoff (9.5 mm/hr to 1.6 mm/hr) , volumes of runoff (55 per cent to 33 per cent of rainfall) and increasing the dry weather flow (9% to 25 % ) & watershed lag time. This is attributed to decreased bed slopes and improved flow channelization. The debris load from both W_1 & W_2 watersheds reduced from near 550 t/ha/yr to about 8 .0 t/ha/yr four years after implementation of interventions.
机译:喜马拉雅山占地面积约50米,发育活动迅速增加。近乎实验性人口增长对已经有限的自然资源进行了进一步的重大需求。垃圾箱从流银行,土地载玻片和矿井废物中的碎片载荷产生,导致流流动制度的平衡,并进一步对生命和财产造成广泛损害。本文涉及 - (a)在喜马拉雅山脉和施瓦温的流域的特征确定,(b),以建立引流区和通道长度上游的通道形态参数之间的关系,以评估管理策略的表现减少径流和碎片负荷生产率。所进行的研究明确建立了 - a)床材料尺寸高达约四分之一至三分之一的洪流长度,其后减少。这种行为是由于血管和引力。 b)频道宽度和本地床坡之间存在反向关系,C)填海措施从近55%降低径流,从550吨/公顷/年到8.0吨/公顷的近55%和碎片。当节约措施得到精心策划并科学实施时,不仅会降低径流和碎片负荷,而且还可以改善干燥的天气流量并维持更长的时间。在位于喜马拉雅山的流域实施时的保护措施证明有效地将径流的峰值(9.5毫米/小时至1.6毫米/小时),径流量(降雨量的55%)和增加干燥天气流量(9%至25%)和流域滞后时间。这归因于床斜坡减少和改善的流动信道。 W_1&W_2流域的碎片负荷从近4年后从接近550 T / HA / Yr减少到约8.0吨/哈/年后的干预措施。

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