首页> 外文期刊>Agriculture, Ecosystems & Environment: An International Journal for Scientific Research on the Relationship of Agriculture and Food Production to the Biosphere >Possibilities of carbon and nitrogen sequestration under conventional tillage and no-till cover crop farming (Mekong valley, Laos).
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Possibilities of carbon and nitrogen sequestration under conventional tillage and no-till cover crop farming (Mekong valley, Laos).

机译:在传统耕作和免耕覆盖耕作法下进行碳和氮固存的可能性(老挝湄公河谷)。

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摘要

There is limited information, particularly in the tropics, of farming systems that loose or accumulate carbon in their soils. We compared no-till with a mulch-providing cover crop with conventional tillage without cover crop. Side effects were also investigated, weeds, surface crusting, soil macrofauna, infiltration, porosity and roots. The study site was a flat sandy clay loam. Treatments were maintained over five years; within this period, the time between the first and last soil sampling was exactly four years. Both times the same profile locations and exactly the same depths were sampled thereby greatly reducing inherent soil variability. Soil was sampled at five increments from 0 to 40 cm depth. The biomass contributions of maize, cover crop and weeds were measured. The main findings were: (1) The cover crop that was alleged to supply extra inputs to the no-till system failed to do so because the weeds in the tillage treatment became as efficient in accumulating biomass as the planted cover crop. (2) With equal organic inputs over four years (43.0 Mg dry weight ha-1 incorporated into the soil under conventional tillage, and 44.2 Mg dry weight ha-1 remaining on the soil surface as mulch under no-till), the tillage system stored (0-40 cm) significantly soil carbon (+590 g C m-2), whereas the no-till lost carbon (-133 g C m-2). The difference between the systems was significant. Carbon accumulated just below the plough layer. Nitrogen stocks remained unchanged. A very significant lowering of the C:N ratio occurred under no-till. The process of transforming the available biomass on the soil surface into organic matter is apparently too slow to avoid direct losses under no-till. Alternatively, ploughing plant residues into the soil enables to capture some of what would otherwise be lost as CO2 through decay, thereby increasing soil carbon. (3) In the last three years of the experiment, maize grain yields and crop residues stabilized at a lower level but were significantly higher under no-till, 16% and 34%, respectively. Higher yields were attributed to more soil water under no-till due to improved soil structure, though bulk density was not affected. The mulch layer protecting the soil surface favoured infiltration by keeping it crust-free. Water availability was further promoted by a better connectivity of pores and more macrofauna. However, the no-till system depended heavily on fertilizers and herbicides. The lack of effectiveness of herbicides against shifting weed communities threatens the continuation of the system.
机译:关于在土壤中散布或积聚碳的耕作系统的信息有限,尤其是在热带地区。我们将免耕与提供覆盖的覆盖作物与传统的无覆盖耕作方式进行了比较。还研究了副作用,杂草,表面结皮,土壤大型动物群,渗透,孔隙度和根系。研究地点是平坦的沙质壤土。治疗维持了五年;在此期间,第一次和最后一次土壤采样之间的时间恰好是四年。两次都采样了相同的剖面位置和完全相同的深度,从而大大降低了土壤固有的变异性。从0到40厘米深度以五个增量对土壤进行采样。测量了玉米,覆盖作物和杂草对生物量的贡献。主要发现是:(1)据称为免耕系统提供额外投入的覆盖作物未能做到这一点,因为耕作处理中的杂草在积累生物量方面与种植的覆盖作物一样有效。 (2)在四年内有机投入相等(常规耕作下将43.0 Mg干重ha -1 掺入土壤,而剩余44.2 Mg干重ha -1 耕作方式覆盖土壤表面)(耕作方式)(0-40 cm)显着增加土壤碳(+590 g C m -2 ),而免耕损失碳(- 133 g C m -2 )。系统之间的差异非常明显。碳堆积在犁层下面。氮库存保持不变。免耕条件下C:N的比率显着降低。将土壤表面可用生物量转化为有机物的过程显然太慢,无法避免免耕法下的直接损失。另外,在土壤中耕作植物残渣可以捕获由于腐烂而以CO 2 的方式损失的一些物质,从而增加土壤碳含量。 (3)在实验的最后三年中,玉米籽粒产量和农作物残渣稳定在较低水平,但在免耕状态下分别显着较高,分别为16%和34%。尽管土壤容重没有受到影响,但由于土壤结构的改善,免耕耕作增加了土壤水的含量,从而提高了产量。保护土壤表面的覆盖层通过保持其无结皮而有利于渗透。更好的孔隙连通性和更多的大型动物群落进一步促进了水的可利用性。但是,免耕制度严重依赖化肥和除草剂。除草剂对杂草群落的转移缺乏效力,这威胁到该体系的持续发展。

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