首页> 外文学位 >Investigating proglacial groundwater systems in the Quilcayhuanca and Yanamarey Pampas, Cordillera Blanca, Peru.
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Investigating proglacial groundwater systems in the Quilcayhuanca and Yanamarey Pampas, Cordillera Blanca, Peru.

机译:调查秘鲁科迪勒拉·布兰卡的Quilcayhuanca和Yanamarey Pampas的地下水生态系统。

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摘要

High-elevation Andean water storage is extremely important for water resources for the arid western coast of South America. Pampas (a subset of paramos) are a freshwater reservoir in the Cordillera Blanca, Peru. These organic-rich clay systems buffer stream and river runoff to the Rio Santa and provide water to surrounding communities. More than 50% of dry season discharge from pampas is groundwater derived, however little is known about their geomorphology and subsurface sedimentology. Watertable measurements, streambed temperature sensors, and ground penetrating radar (GPR) were used to characterize the subsurface and develop a formational model for the Yanamarey and Quilcayhuanca pampas, Cordillera Blanca, Peru.;The water table in July 2009 was found on average to be 0.35 m and 0.57 m below the land surface at Quilcayhuanca and Yanamarey respectively. In the Yanamarey Pampa, streambed temperature sensors showed that upstream, water flows from the stream into the ground and further downstream, water flows upwards recharging the stream. From watertable measurements, a watertable map was produced that showed steeper watertable gradients further up valley. GPR was an effective tool for imaging the subsurface to a depth of 8 meters in the high permittivity material and delineated four stratigraphic units at both sites. In sequence the units are; dry sandy peat soils with pebbles at the surface, water saturated soil with sand and pebbles, linear stratified clay and glacial outwash intermixed with colluviums deposits. The identification of the subsurface sedimentary units allowed for the creation of formation models of both sites. The valley walls of Quilcayhuanca are steeper than Yanamarey, which caused more landslides and consequently more extensive colluvial deposits throughout the Quilcayhuanca valley subsurface. These connected colluvial deposits are likely the primary zone for groundwater flow and storage.
机译:高海拔的安第斯水库对于南美干旱西部海岸的水资源极为重要。南美大草原(帕拉莫斯的一部分)是秘鲁科迪勒拉布兰卡的淡水水库。这些富含有机物的粘土系统缓冲了流向Rio Santa的河流和河流径流,并为周围的社区提供了水。南美大草原上超过50%的旱季排放物是从地下水中提取的,但对其地貌和地下沉积学知之甚少。水位测量,河床温度传感器和探地雷达(GPR)用于表征地下,并为秘鲁科迪勒拉布兰卡的Yanamarey和Quilcayhuanca pampas开发了地层模型; 2009年7月的地下水位平均为Quilcayhuanca和Yanamarey的地面以下分别为0.35 m和0.57 m。在亚纳马里邦邦(Yanamary Pampa),河床温度传感器显示出上游,水从河水流入地面,再往下游,水向上流动,为河水补充水。根据水位测量结果,绘制了水位图,该图显示了更高的山谷水位梯度。 GPR是在高介电常数材料中将地下成像至8米深度的有效工具,并且在两个位置都描绘了四个地层单位。顺序是:干燥的沙质泥炭土表面有卵石,水饱和的土壤有砂石和卵石,线性分层的粘土和冰川冲积物与坡积物混合。通过识别地下沉积单元,可以创建两个站点的地层模型。 Quilcayhuanca的谷壁比Yanamarey陡峭,这引起了更多的滑坡,并因此在整个Quilcayhuanca谷地下形成了更多的砂砾沉积物。这些相连的河床沉积物可能是地下水流动和存储的主要区域。

著录项

  • 作者

    Maharaj, Laura.;

  • 作者单位

    McGill University (Canada).;

  • 授予单位 McGill University (Canada).;
  • 学科 Geology.;Hydrology.
  • 学位 M.Sc.
  • 年度 2011
  • 页码 88 p.
  • 总页数 88
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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