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Quantifying provenance of reservoir sediment using multiple composite fingerprints in an arid region experiencing both wind and water erosion

机译:在风蚀和水蚀的干旱地区使用多个复合指纹对储层泥沙物源进行量化

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摘要

Quantitative information on sediment sources is useful for developing targeted protection measures that effectively control soil erosion in a watershed. In this study, a multiple composite fingerprints method was tested and used for quantifying the sediment provenance of the Danghe River, and for providing effective sediment control strategies for the watershed in an arid region experiencing both wind and water erosion. Surface samples were taken from three geomorphic source areas of dunes, gobi, and upstream mountains; and sediment samples from the watercourses near the reservoir. To accommodate the wide range of sediment size distributions resulting from the fluvial and aeolian processes, sediment contributions from each source were estimated for each of six particle size groups. The results showed that the proportional contributions from each source to the reservoir sediments were 56.73% from upstream mountains, 26.36% from gobi, and 16.91% from dunes, with the relative contributions in each size group following a similar trend. The largest fraction of the sediment was from the 0.063-0.1 mm particle size group, accounting for about 37.09% of the total, in which 4%, 7.59%, and 25.50% were from dunes, gobi, and upstream mountains. Our results also indicated that selective erosion existed in both erosion processes, especially in wind erosion process, and multiple particle size tracking should be used in the cases of severe selective erosion to improve the accuracy of estimation. Also, the sediment contribution rate per unit area was the largest from dunes; thus, controlling wind-blown sand to the river by stabilizing the dunes is recommended to reduce the reservoir siltation. (C) 2019 Elsevier B.V. All rights reserved.
机译:有关沉积物来源的定量信息可用于制定有针对性的保护措施,以有效控制流域的土壤侵蚀。在这项研究中,测试了多种复合指纹方法,并将其用于量化当河的沉积物来源,并为遭受风蚀和水蚀的干旱地区的流域提供有效的沉积物控制策略。表面样本取自沙丘,戈壁和上游山区的三个地貌源区。和水库附近水道的沉积物样本。为了适应河流和风沙过程产生的各种沉积物尺寸分布,对六个粒径组中的每一个估算了每个来源的沉积物贡献。结果表明,每种来源对储层沉积物的比例贡献分别来自上游山峰的56.73%,戈壁滩的26.36%和沙丘的16.91%,每个规模组的相对贡献都遵循相似的趋势。沉积物的最大部分来自0.063-0.1 mm粒径组,约占总量的37.09%,其中4%,7.59%和25.50%来自沙丘,戈壁和上游山区。我们的结果还表明,在两个侵蚀过程中都存在选择性侵蚀,特别是在风蚀过程中,对于严重的选择性侵蚀,应使用多重粒度跟踪以提高估算的准确性。另外,沙丘的单位面积沉积物贡献率最大。因此,建议通过稳定沙丘来控制向河吹风沙,以减少水库淤积。 (C)2019 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《Geomorphology》 |2019年第1期|112-121|共10页
  • 作者单位

    Chinese Acad Sci, Key Lab Desert & Desertificat, Dunhuang Gobi Desert Res Stn, Northwest Inst Ecoenvironm & Resources, Lanzhou 730000, Gansu, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China;

    Chinese Acad Sci, Key Lab Desert & Desertificat, Dunhuang Gobi Desert Res Stn, Northwest Inst Ecoenvironm & Resources, Lanzhou 730000, Gansu, Peoples R China;

    ARS, Grazinglands Res Lab, USDA, El Reno, OK 73036 USA;

    Chinese Acad Sci, Key Lab Desert & Desertificat, Dunhuang Gobi Desert Res Stn, Northwest Inst Ecoenvironm & Resources, Lanzhou 730000, Gansu, Peoples R China;

    Chinese Acad Sci, Key Lab Desert & Desertificat, Dunhuang Gobi Desert Res Stn, Northwest Inst Ecoenvironm & Resources, Lanzhou 730000, Gansu, Peoples R China;

    Chinese Acad Sci, Key Lab Desert & Desertificat, Dunhuang Gobi Desert Res Stn, Northwest Inst Ecoenvironm & Resources, Lanzhou 730000, Gansu, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Multiple composite fingerprints; Sediment provenance; Arid region; Water and wind erosions;

    机译:复合指纹图谱;沉积物出处;干旱区;水和风蚀;

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