首页> 外文期刊>Journal of the Indian Society of Soil Science >Mineralization of Nitrogen, Phosphorus and Sulphur in Soil as Influenced by Rock Phosphate Enriched Compost andChemical Fertilizers
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Mineralization of Nitrogen, Phosphorus and Sulphur in Soil as Influenced by Rock Phosphate Enriched Compost andChemical Fertilizers

机译:富磷堆肥和化肥对土壤氮,磷,硫矿化的影响

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Quantitative information on nutrient mineralization in soil under different nutrient management strategies is essential for better assessment of nutrient availability and their loss from soil. Predicting nutrient mineralization has been one of the greatest challenges to improve nutrient management in agriculture. Laboratory incubation experiment was conducted to study the nitrogen (N), phosphorus (P) and sulphur (S) mineralization in soils amended with rock phosphate (RP) enriched composts and fertilizers over 120 days. Results revealed that RP enriched compost amended soil mineralized higher N and S over unfertilized control. The first-order model was found to be the best suitable for N and S mineralization because it provided the best fit to the experimental data and for its simplicity. Potentially mineralized N (N_0) values ranged from a minimum of 4.0 mg kg~(-1) to a maximum of 52.1 mg kg~(-1) soil and the mineralization rate k varied from 0.023 to 0.052 day1. It was observed that model fittingfor P mineralization did not yield satisfactory results for soil amended with RP enriched compost. The P mineralization study revealed that the soil treated with RP enriched compost showed decline in Olsen-P during the initial stages of 30 days, but improved significantly with the progress of time, indicating that RP enriched compost released P for a longer period which in turn could steadily supply nutrients for longer period for crop growth. The RP enriched compost substantially increased the amountof potentially mineralizable S (S0) and higher rates of S mineralization (k) over unfertilized control.
机译:不同养分管理策略下土壤养分矿化的定量信息对于更好地评估养分的有效性及其从土壤中的流失至关重要。预测养分矿化一直是改善农业养分管理的最大挑战之一。进行了实验室温育实验,研究了用磷岩(RP)富集堆肥和肥料改良的土壤中氮(N),磷(P)和硫(S)的矿化作用,历时120天。结果表明,与未施肥的对照相比,富含RP的堆肥改良后的土壤矿化了较高的N和S。发现一阶模型最适合N和S矿化,因为它为实验数据提供了最佳拟合,并且简单易行。潜在的矿化N(N_0)值范围从最小4.0 mg kg〜(-1)到最大52.1 mg kg〜(-1)土壤,矿化速率k从0.023到0.052天1。观察到,用富含RP的堆肥改良的土壤,磷矿化的模型拟合未获得令人满意的结果。磷矿化研究表明,富含RP的堆肥处理的土壤在30天的初始阶段显示Olsen-P下降,但随着时间的推移显着改善,表明富含RP的堆肥释放P的时间更长。可以长期稳定地供应营养以促进作物生长。与未施肥的对照相比,富含RP的堆肥大大增加了可能矿化的S(S0)的量,并增加了S矿化的速率(k)。

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