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首页> 外文期刊>Quaternary International >Four loess pioneers: Charles Lyell, F. von Richthofen, V.A. Obruchev, LS. Berg
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Four loess pioneers: Charles Lyell, F. von Richthofen, V.A. Obruchev, LS. Berg

机译:黄土的四位先驱者:Charles Lyell,F。von Richthofen,V.A。奥布卢切夫(LS)。山

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The four loess pioneers were Charles Lyell, Ferdinand von Richthofen, Vladimir Obruchev and Lev Berg. Their life spans covered the period 1797-1956. They each contributed significant thoughts and ideas to the development of the study of loess deposits. Their loessic ideas can be related to their life experiences and to their own particular approaches to their chosen branches of science. Their ideas can also be set in a framework of scientific development at a time when scientific knowledge was increasing rapidly and new fields and areas of study were being demarcated. The directions that they indicated and the ideas that they implanted still influence loess research today, and some problems that they touched on remain unresolved. The basic Lyell idea of lacustrine or fluvial deposition followed by uplift held sway from about 1830 till around 1880. Richthofen developed his ideas on aeolian deposition from 1870 and Obruchev developed his ideas after the Potanin expedition, in 1895. Berg offered his concept of loess formation by weathering and soil formation in 1916, and was a keen proponent until his death in 1950. Many scholars offered ideas and proposals on the problem of loess deposit formation but the four chosen individuals appear to predominate, and have delivered the paradigms that have shaped loess research since the 1830s. Richthofen has probably acquired a little too much credit for the aeolian theory, and Obruchev not enough. Obruchev delivered a fully worked out aeolian approach which encompassed post-depositional changes to the loess material. Berg, with his total concentration on post depositional changes was only considering half a picture. Some of his ideas were important but his one eyed view meant that many scholars neglected them. (C) 2016 Elsevier Ltd and INQUA. All rights reserved.
机译:黄土的四个先驱者是查尔斯·莱尔,费迪南德·冯·里希托芬,弗拉基米尔·奥布鲁切夫和列夫·伯格。他们的寿命跨度为1797-1956年。他们各自为黄土矿床研究的发展贡献了重要的思想和观念。他们的黄土思想可能与他们的生活经历以及他们对所选科学学科的独特态度有关。在科学知识迅速增长,新的研究领域和领域被划定之际,也可以在科学发展的框架内设定他们的想法。他们指出的方向和他们所植入的思想至今仍影响着黄土的研究,他们所涉及的一些问题仍未解决。大约1830年至1880年左右,莱尔湖关于湖泊沉积或河流沉积的基本思想一直处于主导地位。里希托芬从1870年开始发展风沙沉积概念,奥布卢切夫在1895年波塔宁探险之后发展了他的思想。伯格提出了黄土形成的概念。在1916年受风化和土壤形成的影响,一直是他的热心拥护者,直到1950年去世。许多学者对黄土沉积物形成问题提出了意见和建议,但四个被选个体似乎占主导地位,并提出了塑造黄土的范例自1830年代开始进行研究。 Richthofen可能对风神学说获得了太多的赞誉,而Obruchev还不够。 Obruchev提出了一种完全可行的风沙方法,其中包括沉积后黄土材料的变化。伯格全神贯注于沉积后的变化,只考虑了一半的照片。他的一些观点很重要,但他的一眼观点意味着许多学者都忽略了它们。 (C)2016 Elsevier Ltd和INQUA。版权所有。

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