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Tillage and manure effect on soil physical and chemical properties and on carbon and nitrogen mineralization potentials

机译:耕作和肥料对土壤理化性质以及碳和氮矿化潜力的影响

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The objective of this work was to study the effects of tillage and liquid manure applications on some physical and chemical properties and also on the carbon and nitrogen mineralization potential from a meadow soil.?Our results indicated that tillage and manure applications had no effect on the concentration of Cu, Mn, total N and organic C in the 0 - 15 cm layer of soil after 15 years of treatment. However soil P, Ca, Mg and Zn contents increased significantly with manure applications. Soil organic matter and total N significantly decreased in the 15 – 30 cm depth. No significant change could be detected in soil structural stability in both layers. Moreover, tillage affected significantly soil soluble C and the C/N ratio. Application of 100 t ha-1?manure significantly increased soil soluble C. The results of this study suggest that tillage increased significantly the soil N mineralization rate. The potentially mineralizable nitrogen (N0) was higher in tilled than in no-tilled soil and was at its maximum in the 0 – 15 cm layer of the soil. Furthermore, a significant positive interaction was observed between tillage and manure application on N mineralized after 1.4 wk (Ne). No significant change was detected in both C mineralization rate (Cm) and potentially mineralizable C (C0). The total amounts of mineralizable carbon (Cm) and nitrogen (Nm) significantly decreased in 15 – 30 cm depth and were very closely correlated with the total amounts of C or N and mineralization rate constants (K).
机译:这项工作的目的是研究耕作和液体肥料施用对某些理化性质以及草甸土壤碳和氮矿化潜力的影响。我们的结果表明,耕作和肥料施用对土壤肥力没有影响。处理15年后,在0-15 cm土层中的Cu,Mn,总氮和有机C的浓度。但是,随着施肥,土壤中的磷,钙,镁和锌含量显着增加。在15 – 30 cm深度,土壤有机质和总氮显着下降。两层土壤结构稳定性均未见明显变化。此外,耕作显着影响了土壤可溶性碳和碳氮比。施100 t ha-1?肥料显着增加了土壤可溶性C。这项研究的结果表明,耕作显着提高了土壤N的矿化速率。耕作过程中潜在的可矿化氮(N0)高于不耕作的土壤,并且在0至15 cm的土壤层中达到最大值。此外,在1.4 wk(Ne)后,在耕作和施肥对氮矿化的氮肥之间存在显着的正向相互作用。 C矿化率(Cm)和潜在矿化C(C0)均未检测到显着变化。在15至30 cm的深度中,可矿化碳(Cm)和氮(Nm)的总量显着下降,并且与C或N的总量以及矿化速率常数(K)密切相关。

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