首页> 外文期刊>Journal of Pure & Applied Microbiology >Tillage, Irrigation Levels and Rice Straw Mulches Effects on Wheat Productivity, Soil Aggregates and Soil Organic Carbon Dynamics After Rice in Sandy Loam Soils of SubtropicalClimatic Conditions
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Tillage, Irrigation Levels and Rice Straw Mulches Effects on Wheat Productivity, Soil Aggregates and Soil Organic Carbon Dynamics After Rice in Sandy Loam Soils of SubtropicalClimatic Conditions

机译:亚热带气候条件下砂壤土上耕作,灌溉水平和稻草覆盖对小麦生产力,土壤团聚体和土壤有机碳动态的影响

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Soil organic carbon is considered to be of central importance in maintaining soil quality. We assessed the adoption of different combinations of tillage, crop residue and irrigation on soil organic carbon (SOC) dynamics in different sized soil aggregates and also on crop yield after 4 years in wheat monoculture field plot experiment in a sandy loam soil under subtropical climatic conditions. Results showed that tillage crop residue and irrigation significantly increased water stable aggregates and had profound effects in increasing the mean weight diameter as well as the formation of macro-aggregates, which were the highest in both surface (14.5 &12.5%) and subsurface (13.4 & 12.1%) soil layers under FIRB and ZT with application rice straw and I5 treatments after 3 years. Hence, better aggregation was found with FIRB with 6t rice straw + I5 where macro-aggregates were greater than 30% of total soil mass. The same treatment also enhanced the labile C and N fractions such as water soluble C, particulate and light fraction organic matter from 7.1 mg-kg1 conventional tillage to 17.6 mg-kg~1 in surface layer and from 6.5 to 16.3 mg-kg~1 in subsurface layer after 3 years leading to the 42% and 39% higher water soluble C stocks over CT in 0-15 cm soil layers, respectively. The changes in water soluble C stocks after 4 years were 45% and 40%. WUE increased as mulching increased for the I2, I3, and I4 treatments, but not for the I5 treatment. We conclude that variants of conservation tillage increase SOCstock in the sandy loam soils of subtropical climatic conditions of western U. P., India and are therefore more sustainable practices than those currently being used.
机译:土壤有机碳被认为对维持土壤质量至关重要。在亚热带气候条件下的沙质壤土小麦单耕田间试验中,我们评估了耕作,作物残渣和灌溉的不同组合对不同尺寸土壤团聚体中土壤有机碳(SOC)动态以及作物单产4年后产量的影响。结果表明,耕作作物残渣和灌溉显着增加了水稳性团聚体,并且对增加平均重量直径和形成大团聚体具有深远的影响,这在表层和地下均最高(分别为14.5%和12.5%)。 3年后,应用稻草和I5处理后,FIRB和ZT下的土壤层增加了13.4%和12.1%)。因此,使用6吨稻草+ I5的FIRB发现更好的聚集,其中宏观聚集大于总土壤质量的30%。相同的处理也将不稳定的C和N组分(如水溶性C,颗粒和轻质组分有机物)从传统耕作的7.1 mg-kg1增加到表层的17.6 mg-kg〜1,从6.5至16.3 mg-kg〜1 3年后地下土壤中的碳含量分别比0-15厘米土壤层中的CT高42%和39%。四年后水溶性碳储量的变化分别为45%和40%。对于I2,I3和I4处理,WUE随着覆盖的增加而增加,但对于I5处理,WUE却没有增加。我们得出的结论是,保护耕作的变种增加了印度西部西部亚热带气候条件下沙质壤土的SOC储量,因此比目前使用的做法更具可持续性。

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