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首页> 外文期刊>Journal of Plant Nutrition >NITROGEN MINERALIZATION POTENTIAL AS INFLUENCED BY MICROBIAL BIOMASS, COTTON RESIDUES AND TEMPERATURE
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NITROGEN MINERALIZATION POTENTIAL AS INFLUENCED BY MICROBIAL BIOMASS, COTTON RESIDUES AND TEMPERATURE

机译:微生物生物量,棉花残留量和温度对氮矿化潜力的影响

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摘要

Integrating information on nitrogen (N) mineralization potentials into a fertilization plan could lead to improved N use efficiency. A controlled incubation mineralization study examined microbial biomass dynamics and N mineralization rates for two soils receiving 56 and 168kg N ha(-1) in a Panoche clay loam (Typic Haplocambid) and a Wasco sandy loam (Typic Torriorthent), incubated with and without cotton (Gossypium hirsutum L.) residues at 10 and 25 degrees C for 203days. Microbial biomass activity determined from mineralized carbon dioxide (CO2) was higher in the sandy loam than in clay loam independent of incubation temperature, cotton residue addition and N treatment. In the absence of added cotton residue, N mineralization rates were higher in the sandy loam. Residue additions increased N immobilization in both soils, but were greater in clay loam. Microbial biomass and mineralization were significantly affected by soil type, residue addition and temperature but not by N level.
机译:将有关氮(N)矿化潜力的信息整合到施肥计划中可以提高氮的利用效率。一项受控孵化矿化研究检查了两种土壤的微生物生物量动态和氮矿化速率,两种土壤分别在Panoche粘土壤土(典型的单倍体)和Wasco砂壤土(典型的Torriorthent)中接受和不与棉花一起孵育,分别接受56和168kg N ha(-1) (Gossypium hirsutum L.)残留物在10和25摄氏度下保持203天。沙质壤土中由矿化二氧化碳(CO2)决定的微生物生物量活性高于黏土壤土,与孵化温度,棉渣添加和氮处理无关。在没有添加棉花残留的情况下,沙壤土中的氮矿化率更高。残留物的添加增加了两种土壤的固氮能力,但在粘土壤土中的固氮能力更高。微生物的生物量和矿化度受土壤类型,残渣添加量和温度的显着影响,但不受氮水平的影响。

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