首页> 外文期刊>Soil Use and Management >Soil organic carbon stock variability in the Northern Gangetic Plains of India: interaction between agro-ecological characteristics and cropping systems
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Soil organic carbon stock variability in the Northern Gangetic Plains of India: interaction between agro-ecological characteristics and cropping systems

机译:印度北部恒河平原土壤有机碳储量变异性:农业生态特征与耕作系统之间的相互作用

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摘要

Soil organic carbon (SOC) content and its spatial distribution in the Northern Gangetic Plain (NGP) Zone of India were determined to establish the cause-effect relationship between agro-ecological characteristics, prevailing crop management practices and SOC stock. Area Spread Index (ASI) approach was used to collect soil samples from the NGP areas supporting predominant cropping systems. Exponential ordinary kriging was found most suitable geo-statistical model for developing SOC surface maps of the NGP. Predicted surface maps indicated that 43.7% area of NGP had 0.5-0.6% SOC, while the rest of the area was equally distributed with high (0.61-0.75%) and low (0.5%) SOC content levels. Averaged across cropping systems, maximum SOC content was recorded in Bhabar and Tarai Zone (BTZ), followed by Central Plain Zone (CPZ), Mid-Western Plain Zone (MWPZ), Western Plain Zone (WPZ) and South-Western Plain Zone (SWPZ) of the NGP. The SOC stock was above the optimum threshold (>12.5Mg/ha) in 97.8, 57.6 and 46.4% areas of BTZ, CPZ and MWPZ, respectively. Only 9.8 and 0.4% area of WPZ and SWPZ, respectively, had SOC stock above the threshold value. The variation in SOC stock was attributed largely to carbon addition through recycling of organic sources, cropping systems, tillage intensity, crop or residue cover and land-use efficiency, nutrient-use pattern, soil texture and prevailing ecosystem. Adoption of conservation agriculture, balanced use of nutrients, inclusion of legumes in cropping systems and agro-forestry were suggested for enhancing SOC stock in the region.
机译:确定了印度北部恒河平原(NGP)区的土壤有机碳(SOC)含量及其空间分布,以建立农业生态特征,现行作物管理实践与SOC存量之间的因果关系。区域扩展指数(ASI)方法用于从支持主要种植系统的NGP地区收集土壤样品。发现指数普通克里金法最适合用于开发NGP的SOC表面图的地统计模型。预测的表面图显示,NGP的43.7%区域具有SOC的0.5-0.6%,而其余区域的SOC含量高(0.61-0.75%)和低(<0.5%)是均匀分布的。在整个作物系统中取平均值,在巴巴和塔莱区(BTZ)记录了最大SOC含量,其次是中部平原区(CPZ),中西部平原区(MWPZ),西部平原区(WPZ)和西南平原区( NGP的SWPZ)。在BTZ,CPZ和MWPZ的97.8、57.6和46.4%的区域中,SOC储量均高于最佳阈值(> 12.5Mg / ha)。 WPZ和SWPZ分别只有9.8和0.4%的面积的SOC储量高于阈值。 SOC储量的变化主要归因于有机资源的循环利用,耕作系统,耕作强度,农作物或残渣覆盖率以及土地利用效率,养分利用方式,土壤质地和普遍的生态系统,从而增加了碳。建议采用保护性农业,平衡利用养分,将豆科植物纳​​入作物系统和农林业,以提高该地区的有机碳储量。

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