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The role of N-15 in tracing N dynamics in agro-ecosystems under alternative systems of tillage management: A review

机译:N-15在耕地管理替代系统下,N-15在农业生态系统中追踪N动态的作用:综述

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Cultivation has led to a substantial loss of soil organic matter in the surface soil layers. The use of no-till (or zero-till) has been promoted as a practice that maximises the retention on organic residues to reverse or slow the loss of soil organic matter. However, the terms are misnomers because sowing the crop disturbs the soil. The definitions of conservation tillage systems should be used, including quantifying the mass of residue return to the system. Over 116 research papers that used N-15 natural abundance, N-15 depleted or N-15 enriched isotopic techniques were reviewed to quantify the impact of tillage, especially no-till, on the N dynamics of cropping systems. The negative effects of no-till on crop yields at low fertiliser N applications were reported in numerous studies that had operated for short periods, with a few conducted on a long-term basis (> 10-15 years). Based on the cumulative research, we concluded that no-till had little impact on N-15 fertiliser recovery, or the accumulation of N released from the mineralisation of "native" soil organic matter. In most studies, the impact of no-till on N dynamics is confounded by soil water and soil temperature differences. Often the positive response to no-till was attributed to greater plant available water during the growing season. Soil moisture was the main determinant of the gross N transformation rate and the potential for N mineralisation was not different between conventional and no-till systems. The effect of no-till is restricted to the surface soil. Although differences exist in the surface soil, we were unable to confirm from the N-15 studies that no-till increased organic N sequestration. Net N mineralisation of the large unlabelled soil organic N pool in the root zone dilutes the effect of increased organic N accumulation and N mineralised in the surface layers of no-till systems. Tillage systems did affect the percentage of legume N derived from the atmosphere. Nitrogen fixation was greater under no-till compared to conventional cultivation when (i) mineral N was lower, and (ii) plant available water status was better due to suppression of weeds.
机译:栽培导致表面土层中的土壤有机物大量损失。使用No-Till(或零率)被促进作为一种做法,最大化有机残留物的保留,以逆转或缓慢土壤有机物丧失。然而,这些术语是错误的,因为播种作物扰乱了土壤。应使用保护耕作系统的定义,包括量化残留物的质量返回到系统。综述了超过116份使用N-15天然丰度,N-15耗尽或N-15富集同位素技术的研究,以量化耕作,特别是No-Till,对种植系统的N个动态的影响。在短期内运营的许多研究中报告了No-Till act over ove operations在低肥料N应用中的负面影响。基于累积研究,我们得出结论,没有对N-15肥料恢复的影响几乎没有影响,或从“天然”土壤有机物的矿化中释放的N释放的N-15。在大多数研究中,通过土壤水和土壤温度差异的禁止N动态的影响。通常对不断增长的季节的阳性反应归因于更多的植物可用水。土壤水分是载体总转化率的主要决定因素,常规和无直接系统之间的N矿化的可能性与N型矿化的可能性不同。 No-Tight的效果仅限于地表土壤。尽管表面土壤中存在差异,但我们无法从N-15研究中确认,但没有增加有机N螯合的研究。根区中大型未标记的土壤有机N池的净矿化稀释了No-Till Systems的表面层中增加了有机N积聚和N矿化的效果。耕作系统确实影响了源自大气层的豆类百分比。与常规培养相比,氮固定在常规培养下更大,当(i)矿物n较低,并且(ii)植物可用水状况较好,由于抑制杂草。

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