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首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Micromorphological and physico-chemical analyses of cultural layers in the urban soil of a medieval city - A case study from Krakow, Poland
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Micromorphological and physico-chemical analyses of cultural layers in the urban soil of a medieval city - A case study from Krakow, Poland

机译:中世纪城市土壤中文化层的微观形态和理化分析-以波兰克拉科夫为例

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This study assessed the impact of human activity on the properties of urban soils and the formation of cultural layers (CLs) over several hundred years by examining the micromorphological, physical and chemical features of those soils. The study relied on a soil profile exposed during archaeological excavations carried out in the Main Market Square (MMS) of Krakow, Poland, in 2007. Two parts of the profile were distinguished. The upper section of the soil profile was composed of 13 cultural layers, while the base layer was composed of macroscopically unchanged natural soil. CLs with similar soil textures clearly differed from the natural horizons (NHs), exhibiting higher organic carbon (C-org), total nitrogen (N-t), CaCO3 and available phosphorus (P-Ol) levels. The ranges of CL C-org, N-t, CaCO3 and Pot levels are 14.3-118 g.kg(-1), 1.1-10.6 g.kg(-1). 10.5-79.0 g.kg(-1) and 163-510 mg.kg(-1), respectively, while NH levels are 039-5.5 g.kg(-1), 0.13-0.54 g.kg(-1), 1.2-2.5 g.kg(-1) and 50.1-214 mg.kg(-1), respectively. CLs were characterised by lower pH values compared to NHs. An A horizon Development Index (ADI) was used to assess the degree of advancement of pedogenesis in the different layers. Additionally, correlation coefficients between ADI and the P-Ol content, as well as between ADI and the C-org content, were calculated.
机译:这项研究通过检查这些土壤的微观形态,物理和化学特征,评估了人类活动对城市土壤特性和文化层(CL)形成的影响,历时数百年。该研究依赖于2007年在波兰克拉科夫的主要市场广场(MMS)进行的考古发掘中暴露的土壤剖面。该剖面的两个部分得以区分。土壤剖面的上部由13个文化层组成,而基础层由宏观上不变的天然土壤组成。具有相似土壤质地的CL与自然界(NHs)明显不同,表现出较高的有机碳(C-org),总氮(N-t),CaCO3和有效磷(P-Ol)含量。 CL C-org,N-t,CaCO3和Pot水平的范围是14.3-118 g.kg(-1),1.1-10.6 g.kg(-1)。 10.5-79.0 g.kg(-1)和163-510 mg.kg(-1),而NH含量分别为039-5.5 g.kg(-1),0.13-0.54 g.kg(-1),分别为1.2-2.5 g.kg(-1)和50.1-214 mg.kg(-1)。 CL的特征在于与NHs相比具有较低的pH值。地平线发展指数(ADI)用于评估不同层中成岩作用的进展程度。另外,计算了ADI与P-Ol含量之间以及ADI与C-org含量之间的相关系数。

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