首页> 外文期刊>Polish Journal of Soil Science >SOIL ORGANIC MATTER STATUS IN AGRICULTURAL SOIL SEQUENCE OF FORMER SHORELINE OF DISAPPEARING SUMOWSKIE LAKES, NORTH-EASTERN POLAND
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SOIL ORGANIC MATTER STATUS IN AGRICULTURAL SOIL SEQUENCE OF FORMER SHORELINE OF DISAPPEARING SUMOWSKIE LAKES, NORTH-EASTERN POLAND

机译:东北波兰消失的苏门斯基湖前线农业土壤序列中土壤有机质的状况

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摘要

The aim of the study has been to define the stocks and the basic properties of soil organic matter in agricultural-used soil sequence located in the former shoreline of disappearing lakes. The study area is located in the catchment of the Sumowskie Lakes, the Brodnica Lake District, North-Eastern Poland. The investigations involved preparation of five soil pits located in the south-western part of the former Sumowskie Lake bottom and on the southern slope of the adjacent kame hill. The greatest soiltransformation is reflected in the quality and quantity of the soil organic matter. Indexes of organic matter quality and TOC stocks are significantly changing along the studied transect. The strongly humidified organic matter is found in mursh horizons.Gyttja layers above the groundwater level have a medium humification index. Horizons saturated with water are very low humidified. TOC stocks drop along the analysed soil sequence from the biogenic plain to the top of the kame hill.
机译:该研究的目的是确定位于消失的湖前海岸线的农业用土壤序列中土壤有机质的储量和基本特性。研究区域位于波兰东北部Brodnica湖区Sumowskie湖的集水区。调查涉及准备五个土壤坑,这些坑位于前Sumowskie湖底部的西南部分和相邻的kame山的南坡上。最大的土壤转化反映在土壤有机质的数量和质量上。有机质质量和TOC储量的指数沿所研究的断面显着变化。在沼泽地带发现了高度增湿的有机质。地下水位以上的Gyttja层具有中等的增湿指数。充满水的地平线湿度非常低。从生物成因平原到龟尾山的顶部,TOC储量沿分析的土壤序列下降。

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