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首页> 外文期刊>The Indian Journal of Agricultural Sciences >Effect of conservation agriculture on soil organic carbon dynamics and mineral nitrogen under different fertilizer management practices in maize (Zea mays)-wheat (Triticum aestivum) cropping system
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Effect of conservation agriculture on soil organic carbon dynamics and mineral nitrogen under different fertilizer management practices in maize (Zea mays)-wheat (Triticum aestivum) cropping system

机译:玉米(ZEA 5月)玉米(Zea Mays)不同肥料管理实践土壤有机碳动力学和矿物氮的影响 - 灌溉系统

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Soil organic carbon (SOC) is the center of all physical, chemical and biological properties of soils, its maintenance and buildup in soils is necessary to sustain the intensive cereal-based cropping system of Indo Gangetic plains. Intensive tillage, residue removal and indiscriminate use of fertilizers led to a continuous deterioration of soil health in Indo Gangetic parts of the country. Under this context, a field experiment on conservation agriculture (CA) was conducted at Taroari, Kamal, comprising four combinations of tillage and residue management [i.e. conventional tillage (CT) with complete residue removal (CT-RR), CT with 20% residue incorporation of wheat, 50% residue incorporation of maize and incorporation of green gram residue (CT+RI+GI), permanent beds (PB) with 20% residue retention of wheat and 50% residue retention of maize (PB+RR), and PB with 20% residue retention of wheat, 50% residue retention of maize and retention of green gram residue (PB+RR+GR)J and three nutrient management options [viz. farmers fertilization practice (FFP), recommended fertilizer dose (RDF) and site-specific nutrient management (SSNM)]. The results showed that, there was an increase in SOC mainly the active SOC pools, permanganate oxidizable-C (1.70 g/kg), hot water extractable-C (0.32 g/kg) and soil microbial biomass C (310 mg/kg) under CA-based treatment (PB+RR+GR) compared to CT (0.58, 0.23 g/kg, 183 mg/kg, respectively). Also, the mineral N was invariably greater under residue treatments. Therefore, crops residue retention as well as balanced fertilization (RDF and SSNM) under CA helped in improving SOC; mineral N and soil aggregation stability which can lead to increased sustainability under cereal-based intensive cropping systems.
机译:土壤有机碳(SOC)是土壤所有物理、化学和生物性质的中心,其在土壤中的维持和积累对于维持印支-恒河平原以谷物为基础的集约种植制度是必要的。密集的耕作、清除残留物和不分青红皂白地使用化肥导致该国印支恒河地区的土壤健康状况持续恶化。在此背景下,在卡马尔的塔罗里进行了保护性农业(CA)田间试验,包括四种耕作和残留物管理组合[即:常规耕作(CT)和完全清除残留物(CT-RR)、CT和50%的小麦残渣掺入、50%的玉米残渣掺入和绿豆残渣掺入(CT+RI+GI)、永久性耕作(PB)和50%的玉米残渣掺入(PB+RR)小麦残留保持率为20%,玉米残留保持率为50%,绿豆残留保持率为(PB+RR+GR)J,以及三种营养管理方案[即农民施肥实践(FFP)、推荐施肥量(RDF)和定点营养管理(SSNM)]。结果表明,与CT(分别为0.58、0.23g/kg、183mg/kg)相比,钙基处理(PB+RR+GR)下土壤有机碳主要增加了活性有机碳库、高锰酸盐可氧化碳(1.70g/kg)、热水可提取碳(0.32g/kg)和土壤微生物生物量碳(310mg/kg)。而且,在残渣处理下,矿质氮含量始终较高。因此,作物残体保持以及钙下平衡施肥(RDF和SSNM)有助于提高土壤有机碳;矿质氮和土壤团聚体的稳定性,在以谷物为基础的集约种植制度下,可以提高可持续性。

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