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首页> 外文期刊>Soil & Tillage Research >Surface soil responses to silage cropping intensity on a Typic Kanhapludult in the piedmont of North Carolina.
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Surface soil responses to silage cropping intensity on a Typic Kanhapludult in the piedmont of North Carolina.

机译:在北卡罗莱纳州山麓的典型的Kanhapludult上,表土对青贮作物种植强度的响应。

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摘要

Although reduced tillage itself is beneficial to soil quality and farm economics, the amount of crop residues returned to the soil will likely alter the success of a particular conservation tillage system within a farm operation. We investigated the impact of three cropping systems (a gradient in silage cropping intensity) on selected soil physical, chemical, and biological properties in the Piedmont of North Carolina, USA. Cropping systems were: (1) maize (Zea mays L.) silage/barley (Hordeum vulgare L.) silage (high silage intensity), (2) maize silage/winter cover crop (medium silage intensity), and (3) maize silage/barley grain - summer cover crop/winter cover crop (low silage intensity). There was an inverse relationship between silage intensity and the quantity of surface residue C and N contents. With time, soil bulk density at a depth of 0-3 cm became lower and total and particulate C and N fractions, and stability of macroaggregates became higher with lower silage intensity as a result of greater crop residue returned to soil. Soil bulk density at 0-3 cm depth was initially 0.88 Mg m-3 and increased to 1.08 Mg m-3 at the end of 7 years under high silage intensity. Total organic C at 0-20 cm depth was initially 11.7 g kg-1 and increased to 14.3 g kg-1 at the end of 7 years under low silage intensity. Stability of macroaggregates at 0-3 cm depth at the end of 7 years was 99% under low silage intensity, 96% under medium silage intensity, and 89% under high silage intensity. Soil microbial biomass C at 0-3 cm depth at the end of 7 years was greater with low silage intensity (1910 mg kg-1) than with high silage intensity (1172 mg kg-1). Less intensive silage cropping (i.e., greater quantities of crop residue returned to soil) had a multitude of positive effects on soil properties, even in continuous no-tillage crop production systems. An optimum balance between short-term economic returns and longer-term investments in improved soil quality for more sustainable production can be achieved in no-tillage silage cropping systems..
机译:尽管减少耕种本身对土壤质量和农场经济有利,但返回土壤的农作物残留量很可能会改变农场运营中特定保护性耕作系统的成功。我们调查了三种耕作制度(青贮作物耕作强度的梯度)对美国北卡罗莱纳州皮埃蒙特市选定土壤的物理,化学和生物学特性的影响。耕作系统是:(1)玉米青贮饲料/大麦青贮饲料(高青贮强度),(2)玉米青贮饲料/冬季覆盖作物(中等青贮强度),和(3)玉米青贮饲料/大麦籽粒-夏季覆盖作物/冬季覆盖作物(青贮强度低)。青贮强度与表面残留碳和氮含量之间存在反比关系。随着时间的流逝,由于更多的农作物残渣返回土壤,因此在0-3 cm深度处的土壤容重降低,总和颗粒C和N分数降低,大集料的稳定性随着青贮强度的降低而提高。在高青贮强度下,0-3 cm深度的土壤容重最初为0.88 Mg m-3,并在7年末增加到1.08 Mg m-3。在低青贮强度下,0-20厘米深度的有机碳总量最初为11.7 g kg-1,并在7年末增加至14.3 g kg-1。在低青贮强度下,大型骨料在7年末在0-3 cm深度处的稳定性为99%,在中等青贮强度下为96%,在高青贮强度下为89%。低青贮强度(1910 mg kg-1)下7年末0-3 cm深度的土壤微生物生物量C比高青贮强度(1172 mg kg-1)更大。低强度青贮作物耕作(即,大量农作物残渣返回土壤)即使在连续的免耕作物生产系统中也对土壤特性产生许多积极影响。免耕青贮作物种植系统可在短期经济收益与长期投资之间保持最佳平衡,以改善土壤质量,实现更可持续的生产。

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