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Impact Of Subsurface Drainage On Nitrogen Transformation And Microbial Activity In A CoastalEcosystem

机译:地下排水对海岸体系中氮转化和微生物活性的影响

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In South-east Asia, coastal tracts are often considered as homogeneous entities in terms of constraints to agricultural production. Most of the lands in these regions, and in India in particular, are saline to saline sodic and are faced with problemsof waterlogging and low carbon content in the root zone. In this study, an attempt is made to understand the nitrogen dynamics in salt-affected coastal rice wetlands that were reclaimed by subsurface drainage. The experimental area consist of fields at various stages of reclamation, equipped with subsurface drains with varying spacing. Date were collected from - four drain spacing/stages of reclamation combinations, namely 15 m (reclaimed), 25 m (reclaimed until1998 and left fallow in 1999 onwards), 35and 55 m (new area under reclamation since 1999), during 1999,2000 and 2001. The area with 25 m spacing was left fallow during 1999 and beyond, and the subsurface drainage system was blocked, to study the accumulation of toxic substance in the root zonein the absence of crops, irrigation, leaching and drainage. The study revealed that subsurface drainage helped to improve the fertility status of the soil by promoting ammonium storage on the clay complex. The process of nitrification was greatly reducedin saline coastal lands due to marginal presence of nitrifiers. Sustained operation of subsurface drainage systems served to maintain a favorable salt content in the upper soil layers, leading to enhanced microbial activity and nitrification. Consequently, nitrite concentration was limited to 0.3 mg l~(-1) in the root zone. Over the three years of the study, there was an exponential increase in the nitrite concentration in the root zone of the 25 m drain spacing area where the drainage system was blocked. Such an increasing trend of nitrite accumulation may give rise to severe nitrite toxicity and other environmental problems. The study concluded with the suggestion that researchers pay attention to nitrite accumulation in coastal land and its subsequent consequence on coastal ecosystems.
机译:在东南亚,在农业生产的限制方面,沿海船舶通常被视为同质实体。大多数这些地区的土地,并在印度尤其是生理盐水盐碱地,面临着problemsof水涝和根区碳含量低。在这项研究中,试图了解由地下排水回收的盐受影响的沿海湿地中的氮动力学。实验区由填海阶段的各个阶段组成,配备有不同间距的地下排水管。从 - 四个排水间隔/阶段收集日期,即15米(回收),25米(1999年回收到1999年的左休耕),35 55米(自1999年以来的填海区),1999,2000 2001年,25米间距的地区在1999年及以后留下了休耕,地下排水系统被封闭,研究了根部中毒物质的积累,没有作物,灌溉,浸出和排水。该研究表明,地下排水有助于通过促进粘土络合物上的铵储存来改善土壤的生育状态。由于氮化物的边际存在,硝化的过程大大降低了盐水沿海地。地下排水系统的持续运行用于在上层土壤层中保持有利的盐含量,导致微生物活性增强和硝化。因此,亚硝酸盐浓度限制在根区中的0.3mg L〜(-1)。在这项研究的三年内,25米漏极间距区域的根区中的亚硝酸盐浓度具有指数增加,其中排水系统被阻断。亚硝酸盐积累的这种趋势可能导致严重的亚硝酸盐毒性和其他环境问题。该研究结束了研究人员对沿海地土地中亚硝酸盐积累的建议及其对沿海生态系统的后果的建议。

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