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Nitrogen fertilizer increased litter deposition and litter N in warm-climate grasslands
Nutrient Cycling in Agroecosystems ( IF 3.1 ) Pub Date : 2021-01-26 , DOI: 10.1007/s10705-021-10119-8
Vanessa Z. Longhini , Abmael S. Cardoso , Andressa S. Berça , Isabel N. O. Carvalho , Robert M. Boddey , Ricardo A. Reis , José C. B. Dubeux , Ana C. Ruggieri

In warm-climate grasslands, litter deposition and decomposition are one of the main pathway of nutrient cycling. The application of nitrogen (N) fertilizer or the inclusion of a legume in such grasslands modifies litter characteristics and chemical composition. This study evaluated how the N supply of palisadegrass [Urochloa brizantha (Hochst. ex A. Rich.) R.D. Webster] pastures affect litter characteristics two years after seeding. Treatments were palisadegrass fertilized or not with N (150 or 0 kg N ha−1 year−1) or mixed with the legume forage peanut (Arachis pintoi cv. Amarillo). The experimental period covered two consecutive rainy seasons. Nitrogen fertilization increased by 43 and 62% the existing litter mass (organic matter, OM), and by 32 and 23% the litter deposition rate compared to unfertilized palisadegrass or legume-grass mixtures, respectively. Both variables were affected by grazing cycle (GC), with low litter deposition rate (14 kg ha−1 d−1 OM) and existing litter mass (1390 kg ha−1 OM) in the GC4 due to low rainfall. Nitrogen fertilized palisadegrass had greater litter N concentration (7.9 ± 0.4 g kg−1 OM—C:N ratio 34 ± 2) than in monoculture or legume-grass mixtures (C:N ratios 45 and 58 ± 2, respectively). Our results indicated that N fertilization of palisadegrass increased litter accumulation, however, N fertilization was not a key driver of the litter decomposition rate, even though it increased litter N concentration. After 2 years of establishment, the proportion of forage peanut in the litter was still low, reducing the benefits of legume inclusion to enhance litter nutrient cycling in these pastures.



中文翻译:

氮肥增加温暖气候草地的凋落物沉积量和氮素

在温暖气候的草原上,凋落物的沉积和分解是养分循环的主要途径之一。在此类草原上施用氮肥或豆科植物会改变凋落物的特性和化学成分。这项研究评估了草木的氮供应(播种后两年)如何影响草木Urochloa brizanthaHochst。ex A. Rich。)RD Webster]草场。处理物palisadegrass受精或不与N(150或O千克氮公顷-1-1)或与豆科牧草花生(混合多年生花生简历。阿马里洛)。实验期连续两个雨季。与未施肥的木瓜草或豆科植物的混合物相比,氮肥的施肥量使现有的凋落物质量(有机物,OM)增加了43%和62%,而凋落物的沉积速率分别增加了32%和23%。这两个变量均受放牧周期(GC)的影响,低降雨的凋落物沉积速率(14 kg ha -1 d -1 OM)和GC4中现有的凋落物质量(1390 kg ha -1 OM)。施氮的木瓜草中的凋落物N浓度更高(7.9±0.4 g kg -1OM-C:N比为34±2),而不是单一培养物或豆类草混合物(C:N比为45和58±2)。我们的结果表明,木瓜的氮肥增加了凋落物的积累,但是,氮肥并不是增加凋落物分解速率的主要驱动力,尽管氮肥增加了凋落物的氮含量。建立两年后,饲草花生在垫料中的比例仍然很低,降低了豆科植物包埋的益处,以增强这些牧场的垫料养分循环。

更新日期:2021-01-28
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