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Vegetation- and Environmental Changes on Non-Reclaimed Spoil Heaps in Southern Poland

机译:波兰南部非再生弃土堆的植被和环境变化

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摘要

The study focused on the changes in vegetation and soils on an undeveloped area of coal mine spoil heaps. The process of vegetation changes was evaluated on the basis of historical cartographic materials and fieldwork. Changes of vegetation in nearly 200 years are presented herein. The main purpose of this study is to present an analysis of spatio-temporal changes in vegetation and their influence on soil features. The diversity of ecological species in terms of habitat requirements, tendency of hornbeam communities formation, and the relationship between forest communities and soil features was found. The basic soil properties were examined under selected plant communities (pH, C , N ), available forms of elements (P, K, Mg), and as plant nutrients and heavy metal occurrence (Fe, Zn, Mn, Co, Cd, Pb, Sr, Cr, Cu). The soil organic carbon (C ) content varied from 3.17 ± 0.007% to 17.7 ± 0.21% and significant differences were observed between sites. The highest total nitrogen (N ) content was recorded in the soils of the sites that were represented by stands (0.60 ± 0.01%). Soil acidity (pH) varied greatly, ranging from acidic (pH = 4.1) to weakly acidic (pH = 5.9). The highest value for Mg (205.43 ± 0.5 mg·kg ) was noted in the soils under (L.) Roth community and for P (184.07 ± 3.77) and K (346.19 ± 2.92 mg·kg ) under the stand. On all sites, Zn was a dominant element and its concentration ranged from 526.1 to 1060.4 mg·kg . Obtained results show how important it is to study the issue of vegetation changes and the formation of the landscape within an industrial city. The described results are important for the management of urban greening issues. Human influence on the disintegration and development of the natural environment is clearly visible. Due to the diversity of former mining areas and their time of creation, the studied area is one of the most important experimental areas for the determination link between vegetation and soil.
机译:该研究侧重于煤矿破坏堆未发达地区植被和土壤的变化。植被变化的过程是在历史制图材料和野外工作的基础上进行评估。本文介绍了近200年植被的变化。本研究的主要目的是分析植被的时空变化及其对土壤特征的影响。在栖息地要求方面,生态物种的多样性,发现了角化社区形成的趋势,以及森林社区与土壤特征的关系。在选定的植物社区(pH,C,N)下,可用的元素(P,K,Mg)和植物营养和重金属发生(Fe,Zn,Mn,Co,Cd,CD,Pb ,sr,cr,cu)。土壤有机碳(C)含量从3.17±0.007%变化至17.7±0.21%,位点之间观察到显着差异。最高总氮气(N)含量被记录在由展位表示的位点的土壤中(0.60±0.01%)。土壤酸度(pH)大大变化,从酸性(pH = 4.1)到弱酸(pH = 5.9)。在(L.)罗斯群落下的土壤中,在架子下(184.07±3.77)和K(346.19±2.92 mg·kg),在土壤下,在土壤中达到最高值(205.43±0.5mg·kg)。在所有地点,Zn是一个主要的元素,其浓度范围为526.1至1060.4 mg·kg。获得的结果表明,研究植被变化问题以及工业城市内景观的形成是多么重要。所描述的结果对城市绿化问题的管理很重要。人们对崩解和自然环境的发展的影响清晰可见。由于前采矿区的多样性及其创作的时间,研究区是植被和土壤中最重要的实验领域之一。

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