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Factors determining soil microbial biomass and nutrient immobilization in desert soils

机译:决定荒漠土壤微生物生物量和养分固定化的因素

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We examined the 10-day response of soil microbial biomass-N to additions of carbon (dextrose) and nitrogen (NH4NO3) to water-amended soils in a factorial experiment in four plant communities of the Chihuahuan desert of New Mexico (U.S.A.). In each site, microbial biomass-N and soil carbohydrates increased and extractable soil N decreased in response to watering alone. Fertilization with N increased microbial biomass-N in grassland soils; whereas, fertilization with C increased microbial biomass-N and decreased extractable N and P in all communities dominated by shrubs, which have invaded large areas of grassland in the Chihuahuan desert during the last 100 years. Our results support the hypothesis that the control of soil microbial biomass shifts from N to C when the ratio of C to N decreases during desertification.
机译:我们在美国新墨西哥州奇瓦瓦沙漠的四个植物群落的因子实验中研究了土壤微生物生物质-N对碳(葡萄糖)和氮(NH4NO3)添加对水改性土壤的10天响应。在每个地点,微生物生物量-N和土壤碳水化合物增加,可提取土壤氮减少,仅响应浇水。施氮肥增加了草地土壤微生物生物量-N;然而,在过去100年中,灌木入侵了奇瓦瓦沙漠大片草原的灌木群落中,C施肥增加了微生物生物量-N,减少了可提取的N和P。我们的研究结果支持了这样一种假设,即当荒漠化过程中C/N比降低时,土壤微生物生物量的控制由N转移到C。

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