首页> 外文期刊>Crop & Pasture Science >Soil organic carbon concentrations and storage in irrigated cotton cropping systems sown on permanent beds in a Vertosol with restricted subsoil drainage. (Special Edition: Cotton Catchment Communities CRC - research outcomes & innovation (Part 1).)
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Soil organic carbon concentrations and storage in irrigated cotton cropping systems sown on permanent beds in a Vertosol with restricted subsoil drainage. (Special Edition: Cotton Catchment Communities CRC - research outcomes & innovation (Part 1).)

机译:灌溉棉花种植系统中土壤有机碳的浓度和存储播种在Vertosol的固定床中,并限制了土壤的下层排水。 (特别版:棉花流域社区CRC-研究成果与创新(第1部分)。)

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Long-term studies of soil organic carbon dynamics in two- and three-crop rotations in irrigated cotton (Gossypium hirsutum L.) based cropping systems under varying stubble management practices in Australian Vertosols are relatively few. Our objective was to quantify soil organic carbon dynamics during a 9-year period in four irrigated, cotton-based cropping systems sown on permanent beds in a Vertosol with restricted subsoil drainage near Narrabri in north-western New South Wales, Australia. The experimental treatments were: cotton-cotton (CC); cotton-vetch (Vicia villosa Roth. in 2002-06, Vicia benghalensis L. in 2007-11) (CV); cotton-wheat (Triticum aestivum L.), where wheat stubble was incorporated (CW); and cotton-wheat-vetch, where wheat stubble was retained as in-situ mulch (CWV). Vetch was terminated during or just before flowering by a combination of mowing and contact herbicides, and the residues were retained as in situ mulch. Estimates of carbon sequestered by above- and below-ground biomass inputs were in the order CWV CW=CV > CC. Carbon concentrations in the 0-1.2 m depth and carbon storage in the 0-0.3 and 0-1.2 m depths were similar among all cropping systems. Net carbon sequestration rates did not differ among cropping systems and did not change significantly with time in the 0-0.3 m depth, but net losses occurred in the 0-1.2 m depth. The discrepancy between measured and estimated values of sequestered carbon suggests that either the value of 5% used to estimate carbon sequestration from biomass inputs was an overestimate for this site, or post-sequestration losses may have been high. The latter has not been investigated in Australian Vertosols. Future research efforts should identify the cause and quantify the magnitude of these losses of organic carbon from soil.
机译:在澳大利亚Vertosols中,在不同的茬茬管理实践下,基于灌溉棉(Gossypium hirsutum L.)的耕作系统在两次和三次作物轮作中土壤有机碳动力学的长期研究相对较少。我们的目标是在澳大利亚新南威尔士州西北部的Narrabri附近的Vertosol种植于永久土壤中的四个灌溉,棉花基种植系统中,对9年内的土壤有机碳动态进行量化。实验处理是:棉-棉(CC);棉v(Vicia villosa Roth。2002-06,Vicia benghalensis L. 2007-11)(CV);掺有麦茬(CW)的棉麦(Triticum aestivum L.);以及小麦-紫wheat菜,其中麦茬留作原地覆盖(CWV)。通过割草和接触除草剂的组合,紫etch在开花期间或开花前即终止,残留物保留为原地覆盖。地上和地下生物量输入所固存的碳的估算顺序为CWV CW = CV> CC。在所有耕作系统中,深度为0-1.2 m的碳浓度和深度为0-0.3和0-1.2 m的碳储量相似。耕作制度中的净碳固存率没有差异,在0-0.3 m深度不会随时间显着变化,但在0-1.2 m深度会发生净损失。固存碳的测量值与估计值之间的差异表明,用于估算来自生物量输入的碳固存的5%的值对于该地点而言是高估了,或者固存后的损失可能很高。后者尚未在澳大利亚Vertosols中进行调查。未来的研究工作应查明原因并量化土壤中有机碳损失的程度。

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