喀尔巴阡山脉罕见的灰熊

N. Băcăinţan, Vl. Perepeliță, Gh. Șandor
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引用次数: 0

摘要

如果知道环境条件的特点,就可以很好地预测某一地区某一土壤类型的发生。除了其他因素外,预测的准确性还会受到以下事实的影响:有时,一些土壤出现在非典型条件下,很少满足条件。这些突发事件引起了人们对土壤发生的一些因素的作用方式和灾害在土壤覆盖层形成中的作用认识不足的注意。为了更好地理解喀尔巴阡山脉灰长岩的成因,我们将介绍两种罕见的情况:中度陡坡上的灰长岩和石灰岩上的灰长岩。在弗朗西亚山脉(东喀尔巴阡山脉),我们在海拔1400 - 1500米的斜坡上发现了20 - 35%的灰泥(在砂岩上);在布塞吉山脉(经向喀尔巴阡山脉),我们在海拔约2120米的石灰岩上发现了灰泥。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
RARE OCCURRENCES OF PODZOLS FROM THE CARPATHIANS
The occurrence of a soil type in a certain area may be predicted satisfactorily if the characteristics of the environmental conditions are well known. The accuracy of the prediction is altered - among other things - by the fact that, sometimes, some soils appear in atypical conditions, rarely met. These unexpected occurrences are drawing our attention to the insufficient understanding of the way some factors of soil genesis function and to the role of the hazard in the building of soil covering. For a better understanding of the genesis of the podzols from the Carpathians we are going to present two cases of rare occurrences: podzols on moderate - steep slopes and podzols on limestone. In the Vrancea Mountains (the Eastern Carpathians) we found podzols (on sandstones) on slopes of 20 - 35 %, at 1400 - 1500 m a.s.l; in the Bucegi Mountains (the Meridional Carpathians) we found podzols on limestone, at about 2120 m a.s.l.
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