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Changes in microbial biomass and activity in relation to shifting cultivation and horticultural practices in subtropical evergreen forest ecosystem of north-east India

机译:印度东北亚热带常绿森林生态系统中微生物生物量和活性的变化与种植和园艺实践的变化有关

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The present study conducted in the Nokrek biosphere reserve (BR) of Meghalaya in north-east India aimed at analyzing the impact of human activities such as shifting agriculture ('Jhum') and horticultural practices on temporal and spatial changes in microbial biomass and dehydrogenase and urease activities in soil. Microbial biomass-C (MBC) and -N(MBN) as well as dehydrogenase and urease activities were significantly (P < 0.01) greater in the soils of the undisturbed forest ecosystem in core zone of the BR than the soils under various land use practices in the buffer zone of the BR. The microbial biomass-N in the surface soil layer (0-10 cm) was maximum (285.4 mu g g(-1)) in the undisturbed core zone and minimum (75.1 mu g g(-1)) in the 1-year-old jhum fallow, which was subjected to intense human activities. Similarly, dehydrogenase (TPF released = 0.70 mu g g(-1) 24 h(-1)) and urease activities (NH4 released = 31.56 mu g 100 g(-1) 6 h(-1)) were maximum in the undisturbed core zone and minimum (TPF released = 0.37 mu g g(-1) 24 h(-1) and NH4 released = 10.78 mu g 100 g(-1) 6 h(-1), respectively) in the 1-year-old jhum fallow. Thus, human activities in the buffer zone of the BR were responsible for significant reduction in both microbial biomass-N and enzyme activities. Both these properties showed recovery during regrowth of vegetation on jhum fallows. Microbial biomass-N and enzyme activities declined significantly (P < 0.01) with increasing soil depth at all the sites. Seasonal variations in both microbial biomass-N and enzyme activities at all sites were also significant (P < 0.01) with peak in autumn and trough in winter. (c) 2005 Elsevier SAS. All rights reserved.
机译:本研究是在印度东北部梅加拉亚邦的Nokrek生物圈保护区(BR)进行的,旨在分析人类活动的影响,例如农业转移(Jhum)和园艺实践对微生物生物量和脱氢酶的时空变化的影响。土壤中的脲酶活性。在不同土地利用方式下,BR核心区未受干扰的森林生态系统土壤中的微生物生物量-C(MBC)和-N(MBN)以及脱氢酶和脲酶活性显着(P <0.01)在BR的缓冲区。在1年生的土壤中,表层土壤层(0-10 cm)的微生物生物量氮最大(285.4 mu gg(-1)),最小(75.1 mu gg(-1))。 jhum休闲,这是人类的活动。同样,脱氢酶(释放的TPF = 0.70μggg(-1)24 h(-1))和脲酶活性(释放的NH4 = 31.56μg100 g(-1)6 h(-1))在未干扰的核中最大区域和最小值(1岁jhum)(TPF释放分别为0.37 mu gg(-1)24 h(-1)和NH4释放分别为10.78μg 100 g(-1)6 h(-1))休耕。因此,BR缓冲带中的人类活动导致微生物生物量N和酶活均显着降低。这两种特性均显示出在草场休耕期间植被恢复期间的恢复。在所有地点,随着土壤深度的增加,微生物量氮和酶活性显着下降(P <0.01)。在所有地点,微生物生物量氮和酶活性的季节性变化也很明显(P <0.01),秋季为高峰,冬季为低谷。 (c)2005 Elsevier SAS。版权所有。

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