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Changes in permafrost ecosystem under the influences of human engineering activities and its enlightenment to railway construction

机译:人类工程活动影响下的多年冻土生态系统变化及其对铁路建设的启示

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Through the investigations of sample belt transects and sample quadrats, the variation characteristics of the disturbed ecosystem by highway engineering in the permafrost region along the Qinghai-Tibet highway line were studied from the ecological elements such as permafrost ecosystem, community type, biodiversity and biological productivity and biological habitat conditions including soil environmental conditions and permafrost environmental conditions. The results show that in the sense of biology the restoration of high-cold steppe ecosystem was much better than that of high-cold meadow ecosystem after nearly 25 a of natural reconversion. This is mainly manifested in several respects: The dominant plant species of the high-cold steppe have occurred or even held a predominant position; local zonal biodiversity and population abundance have reached or even exceeded the level of the undisturbed natural steppe system. Viewed from soil environment change, organic matter content in the disturbed high-cold steppe on an average decreased by 61.5 percent and total N content decreased by 52.51 percent, but the nutrient regime of surface soil layer in most of the region corresponded to that of main grassland soil types in the arid region, which is favourable to the growth of cold-resistant species. The mean nutrient contents of the disturbed high-cold meadow soil (Gelic cambosols) were higher than those of natural cryic aridsols. The maintenance of the integrity of meadow soil structure is crucial to the restoration of high-cold meadow ecosystem. However, the distribution and maintenance of high-cold meadow ecosystem were closely related to the permafrost environment, the restoration degree of the disturbed high-cold steppe ecosystem did not show an obvious restrictive relation with permafrost environment. Once the permafrost environment was destroyed by the engineering activities, the high-cold meadow ecosystem was very difficult to rehabilitate. From the comparison of the variation laws of the ecosystem along the Qinghai-Tibet highway line, the authors put forward two enlightenments for the eco-environmental protection in the construction processes of the Qinghai-Tibet railway.
机译:通过对样带样带和样方的调查,从多年冻土生态系统,群落类型,生物多样性和生物生产力等生态要素出发,研究了青藏公路沿线多年冻土地区公路工程扰动生态系统的变化特征。生物栖息地条件,包括土壤环境条件和多年冻土环境条件。结果表明,在生物学意义上,经过近25 a的自然转化,高寒草原生态系统的恢复比高寒草甸生态系统的恢复要好得多。这主要表现在以下几个方面:高寒草原的优势植物已经出现,甚至占据了主导地位;当地的区域生物多样性和人口数量已经达到甚至超过了未受干扰的自然草原系统的水平。从土壤环境变化看,受干扰的高寒草原有机质含量平均下降61.5%,总氮含量下降52.51%,但大部分地区表层土壤养分状况与主要土壤保持一致。干旱地区的草地土壤类型有利于耐寒物种的生长。受干扰的高寒草甸土壤(Gelic cambosols)的平均养分含量高于天然的冰冻干旱地区。维持草地土壤结构的完整性对于恢复高寒草甸生态系统至关重要。然而,高寒草甸生态系统的分布与维持与多年冻土环境密切相关,受干扰的高寒草原生态系统的恢复程度与多年冻土环境没有明显的制约关系。工程活动破坏了永久冻土环境后,高寒草甸生态系统就很难恢复。通过对青藏公路沿线生态系统变化规律的比较,对青藏铁路建设过程中的生态环境保护提出了两个启示。

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