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Long-term application effects of chemical fertilizer and compost on soil carbon under intensive rice-rice cultivation

机译:水稻精耕细作中化肥和堆肥对土壤碳的长期施用效应。

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From a long-term fertilizer experiment on rice-rice cropping in Typic Endoaquept, established at the Central Rice Research Institute, Cuttack, India in 1969, effects of application of composted manure (5 Mg ha(-1) year(-1)) and chemical fertilizers (N, NP, NK, and NPK twice in a year), in series without compost (C-0) or with compost (C-1) on changes in soil carbon and microbial pools were examined by comparing the soils archived in 1984 and those sampled in 2004. Mean concentrations of soil organic carbon (SOC) varied between 5.5 and 7.6 g kg(-1) in 1984, and 6.8 and 10.8 g kg(-1) in 2004, respectively. Temporal increases in the total amounts of carbon, which reflect the carbon sequestration potential of the soil followed the order: C-1 + NK > C-1 + NP = C-1 + NPK > C-1 + N = C-1-control > C-0 + NP = C-0 + NK > C-0 + NPK > C-0-control > C-0 + N. Fractions of H2O-C and K2SO4-C were higher in 1984, especially in those soil treated without compost. A reverse trend was observed in case of KMnO4-C and carbohydrate-C fractions. The continuous application of compost enhanced microbial biomass carbon as well as active microbial biomass carbon in 2004. Long-term application of chemical fertilizers in combination, rather than N alone, had beneficial effects on soil carbon and microbial pools. Compost application, even once a year, invariably led to higher increments in both soil carbon and microbial pools and the combinations of chemical fertilizers with compost generally showed comparable effects in the long-term.
机译:根据1969年在印度Cuttack中央水稻研究所建立的Typic Endoaquept水稻水稻长期作肥试验,施用堆肥的效果(5 Mg ha(-1)年(-1))通过比较存档的土壤,检查了无堆肥(C-0)或有堆肥(C-1)的土壤中碳和微生物库变化的化学肥料和化学肥料(每年两次,每年两次,分别用于N,NP,NK和NPK)分别于1984年和2004年取样。土壤有机碳(SOC)的平均浓度在1984年为5.5至7.6 g kg(-1)之间,在2004年为6.8至10.8 g kg(-1)之间。碳总量的时间增加,反映了土壤的固碳潜力,其顺序为:C-1 + NK> C-1 + NP = C-1 + NPK> C-1 + N = C-1-对照> C-0 + NP = C-0 + NK> C-0 + NPK> C-0对照> C-0 + N.1984年H2O-C和K2SO4-C的馏分较高,尤其是在那些土壤中未经堆肥处理。在KMnO4-C和碳水化合物-C馏分的情况下,观察到相反的趋势。 2004年,堆肥的连续施用增强了微生物生物量碳和活性微生物生物量碳。长期施用化肥而不是单独使用氮肥,对土壤碳和微生物库产生了有益影响。即使每年施用堆肥,也总是导致土壤碳库和微生物库的增加,而且从长期来看,化学肥料与堆肥的组合通常显示出可比的效果。

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