Results of the study of pH and organic matter in the surface soil of Ulaanbaatar

Byambasuren Tsagaan, Ochirbat Ganbaatar, Azzayaa Otgonbayar
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Abstract

This work summarizes the results of a study into such important urban soil parameters as soil actual (pH) and potential acidity (pH) and soil organic matter content (SOM) in the surface soil of Ulaanbaatar. The soil pH in Ulaanbaatar is slightly alkaline, with a median pH value of 7.36 (actual acidity) and 6.93 (potential acidity), and they were found to be the highest in the industrial zone as compared to other zones in the city. The median value of organic matter content in Ulaanbaatar surface soil was 5.61%, with a high variability in the industrial (C.V.-119%) and transport (C.V.-55.34%) zones. The SOM mean value in urban soil is less than the background value in surface soil from natural area, indicating to increasing compaction and reduction of porosity of soil in urban areas. Also, organic matter content have decreased relatively to previous data, reflecting the urbanization process and such long-term processes as aerial urban fallout.
乌兰巴托市表层土壤pH和有机质的研究结果
本工作总结了乌兰巴托表层土壤中土壤实际酸度(pH)、潜在酸度(pH值)和土壤有机质含量(SOM)等重要城市土壤参数的研究结果。乌兰巴托的土壤pH值为微碱性,中值pH值为7.36(实际酸度)和6.93(潜在酸度),与该市其他地区相比,工业区的土壤pH最高。乌兰巴托表层土壤有机质含量的中值为5.61%,在工业区(C.V.-119%)和运输区(C.V.-55.34%)变化较大。城市土壤SOM平均值小于自然区表层土壤的背景值,表明城市土壤的压实度增加,孔隙率降低。此外,有机物含量与以前的数据相比有所下降,反映了城市化过程和城市上空沉降等长期过程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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