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首页> 外文期刊>Forest Ecology and Management >Interactive influences of silvicultural management and soil chemistry upon soil microbial abundance and nitrogen mineralization.
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Interactive influences of silvicultural management and soil chemistry upon soil microbial abundance and nitrogen mineralization.

机译:营林管理和土壤化学对土壤微生物丰度和氮矿化的互动影响。

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An investigation was made possible interactive effects between soil acidification (a widespread, chronic mode of disturbance) and forest thinning (a site specific acute disturbance) to determine whether such a mechanism was capable of producing changes in more general ecosystem properties and processes. Two experimental forest sites (mixed broadleaved forest dominated by Quercus spp.) in the Daniel Boone National Forest, Kentucky, USA, with similar history, management, and parent material, but differing soil acidity (soil pH 4.4 and 5.1) were selected for the study. An analysis of NO3 and NH4 deposition at the 2 sites from 1984 to 1995, showed that they had similar N deposition histories. At each forest site 2 plots that were experimentally thinned in the 1960s, and 2 adjacent unmanaged plots, were sampled for soil chemical characteristics, microbial abundance, N mineralization and nitrification. There were significant differences between forest sites and significant effects of management for allsoil chemical parameters, fungal biomass, N mineralization and nitrification. Soils from managed plots were generally higher in pH, nutrient availability and nitrification rates. There were significant interactions between site and management for NO3, pH, Ca, Ca:Al ratio and nitrification, resulting from the greater magnitude of the management effect at the less acidified site. Additionally, there were interactive effects of site and management in organic C, NH4 and fungal hyphal length, because plotsat the 2 sites showed dissimilar effects of management. Modelling using path analysis determined that N mineralization was most strongly predicted by combinations of organic C, Al, Ca:Al ratio, and fungal:bacterial ratio, while inorganic N availability and Ca:Al ratio were the main factors for nitrification. Fungal hyphal length was most strongly predicted by Al and pH; in contrast, path analysis failed to produce a model for bacterial abundance. These results suggest (1) that acute and chronic modes ofdisturbance have the potential to interact in a significant and ecologically meaningful manner and (2) that research to assess forest health should be based on key ecosystem processes, such as N mineralization and nitrification.
机译:研究使土壤酸化(一种广泛的,长期的干扰模式)和森林稀疏化(一种特定地点的急性干扰)之间的相互作用成为可能,以确定这种机制是否能够在更普遍的生态系统特性和过程中产生变化。在美国肯塔基州丹尼尔布恩国家森林中的两个实验林地(以栎属为主的混合阔叶林),具有相似的历史,管理和母本,但土壤酸度不同(土壤pH 4.4和5.1)。研究。对1984年至1995年这两个站点的NO3和NH4沉积进行的分析表明,它们具有相似的N沉积历史。在每个森林站点,采样了2个在1960年代进行了实验性稀疏的土地和2个相邻的非管理土地,以获取土壤化学特征,微生物丰度,氮矿化和硝化作用。森林地点之间存在显着差异,而土壤化学参数,真菌生物量,氮矿化和硝化作用的管理效果显着。受管理地块的土壤的pH值,养分利用率和硝化率通常较高。在NO3,pH,Ca,Ca:Al比和硝化作用的位点与管理之间存在显着的相互作用,这是由于酸化程度较低的位点的管理效果更大。此外,在有机碳,NH4和真菌菌丝长度中,位点和管理存在交互作用,因为这两个位点的样地显示出不同的管理作用。使用路径分析的模型确定,有机碳,铝,钙:铝比和真菌:细菌比的组合最能预测氮矿化,而无机氮的有效性和钙:铝比是硝化的主要因素。 Al和pH最强烈地预测真菌菌丝长度。相反,路径分析无法产生细菌丰度的模型。这些结果表明(1)急性和慢性干扰模式有可能以重要且对生态有意义的方式相互作用,并且(2)评估森林健康的研究应基于关键的生态系统过程,例如氮矿化和硝化。

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