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Effects of glacial-interglacial climate change on mass wasting, southeastern Minnesota.

机译:明尼苏达州东南部冰川-冰川间气候变化对整体浪费的影响。

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摘要

Glacial-interglacial changes in mass wasting in the lower Root River basin, southeastern Minnesota, were investigated using a combination of field stratigraphy and sedimentology, analyses of mass movement mechanics, and numerical modelling of soil heat and water flow. Most deposits in the study area are interpreted as products of mass wasting. Some are specifically attributed to solifluction; the mass wasting processes responsible for other depositional units cannot be determined from the field evidence. Radiocarbon dates, inclusion of silt reworked from loess units of known age, stratigraphic relationships with late Wisconsinan fluvial sediment, and geomorphic relationships with the late Wisconsinan Savanna Terrace, all indicate that most mass wasting deposits in the study area are Wisconsinan. Mass wasting began some time before 25,000 14C yr B.P., and continued until at least 13,580 O 60 14C yr B.P. (Beta-82839). There is little evidence of Holocene mass wasting on major valley-wall slopes, except possible slow soil creep.; Slope stability analyses indicate that clast-supported diamictons mantling many steep slopes in the study area should not be susceptible to rapid sliding failure even if saturated to the surface. This provides an explanation for the Holocene stability of these slopes. This result also supports interpretation of these diamictons as solifluction deposits, rather than the product of rapid flows, although deposition by rapid flows is suggested by clast fabrics.; Numerical modelling simulations of soil moisture and ground frost regime were carried out using paleoclimatic scenarios for 21 ka, 16 ka, and 14 ka, based on general circulation model output. Permafrost develops under the 21 ka paleoclimatic scenario, and this leads to a major increase in soil wetness and frost heave potential. This supports the hypothesis that permafrost development was the specific factor responsible in large part for the late Wisconsinan mass wasting episode.
机译:利用田间地层学和沉积学,质量运动力学分析以及土壤热和水流动的数值模型,研究了明尼苏达州东南部罗特河下游流域冰川消融的冰川间变化。研究区域中的大多数沉积物被解释为大量浪费的产物。有些特别归因于唯独;无法根据现场证据确定造成其他沉积单元的大量浪费过程。放射性碳年代,从已知年龄的黄土单元返工的泥沙,与威斯康星州晚期河流沉积物的地层关系以及与威斯康星州萨凡纳阶地晚期的地貌关系,都表明该研究区中大部分的浪费矿床都是威斯康星州。大规模浪费开始于BPM 25,000 14C之前的某个时间,并持续到至少13580 O 60 14C B.P. B.P.。 (Beta-82839)。除可能缓慢的土壤蠕变外,很少有证据表明全新世物质在主要的谷壁斜坡上浪费。边坡稳定性分析表明,研究区域内许多陡峭斜坡所支撑的支撑有裂痕的双曲子即使表面饱和也不应遭受快速滑动破坏。这为这些斜坡的全新世稳定性提供了解释。该结果也支持将这些双嘧啶解释为固溶沉积物,而不是快速流动的产物,尽管用增粘织物建议通过快速流动进行沉积。基于常规循环模型输出,使用古气候情景对21 ka,16 ka和14 ka进行了土壤水分和地面霜冻状况的数值模拟。多年冻土在21 ka古气候情景下发展,这导致土壤湿度和霜冻潜能的大大增加。这支持了以下假设:多年冻土的形成是造成威斯康星州后期大规模消减事件的主要原因。

著录项

  • 作者

    Mason, Joseph A.;

  • 作者单位

    The University of Wisconsin - Madison.;

  • 授予单位 The University of Wisconsin - Madison.;
  • 学科 Physical Geography.; Geology.
  • 学位 Ph.D.
  • 年度 1995
  • 页码 366 p.
  • 总页数 366
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 自然地理学;地质学;
  • 关键词

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