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首页> 外文期刊>Environment and History >The Origins of the Russian Chernozem Soil (Black Earth): Franz Joseph Ruprecht's 'Geo-Botanical Researches into the Chernozem' of 1866
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The Origins of the Russian Chernozem Soil (Black Earth): Franz Joseph Ruprecht's 'Geo-Botanical Researches into the Chernozem' of 1866

机译:俄罗斯黑猩猩土壤(黑土)的起源:弗朗兹·约瑟夫·鲁普雷希特(Franz Joseph Ruprecht)1866年的“对黑黑猩猩的地球植物学研究”

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摘要

This article analyses the contribution of the Austrian-born Russian scientist, Franz Joseph Ruprecht (1814-70) to the development of geobotany in general and to the controversial issue of the origins of the very fertile chernozem (Black Earth) of the steppe region of the Russian Empire. On the basis of careful field work and microscopic analysis of samples of chernozem, Ruprecht argued, in an important article published in St Petersburg in 1866, that the organic matter in the soil was decomposed steppe grasses. Thus, the chernozem was of steppe origins, not forest or peat as had been assumed by most scientists prior to his researches. Ruprecht's work laid the basis for the later, and better known, work on the chernozem by pioneering soil scientist Vasilii Dokuchaev (1846-1903). The article places Ruprecht's researches in the context of contemporary social, economic, and political as well as scientific developments.
机译:本文分析了出生于奥地利的俄罗斯科学家弗朗兹·约瑟夫·鲁普雷希特(Franz Joseph Ruprecht,1814-70)对地质植物学的总体发展以及该地区草原肥沃的黑钙土(黑土)起源的争议性问题的贡献。俄罗斯帝国。鲁普雷希特在认真的野外工作和对黑钙土样品的微观分析的基础上,于1866年在圣彼得堡发表的重要文章中指出,土壤中的有机物被分解为草原草。因此,黑钙质起源于草原,而不是大多数科学家在研究之前所假设的森林或泥炭。鲁普雷希特(Ruprecht)的工作为先驱土壤科学家Vasilii Dokuchaev(1846-1903)后来在黑钙土上的研究奠定了基础。本文将Ruprecht的研究放在当代社会,经济,政治以及科学发展的背景下。

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