Human activities have greatly increased the availability of biologically active forms of nutrients [e.g., nitrogen (N), phosphorous (P), potassium (K), magnesium (Mg)] in many soil ecosystems worldwide. Multi-nutrient fertilization strongly increases plant productivity but may also alter the storage of carbon (C) in soil, which represents the largest terrestrial pool of organic C. Despite this issue is important from a global change perspective, key questions remain on how the single addition of N or the combination of N with other nutrients might affect C sequestration in human-managed soils. Here, we use a 19-year old nutrient addition experiment on a permanent grassland to test for nutrient-induced effects on soil C sequestration. We show that combined NPKMg additions to permanent grassland have ‘constrained’ soil C sequestration to levels similar to unfertilized plots whereas the single addition of N significantly enhanced soil C stocks (N-only fertilized soils store, on average, 11 t C ha−1 more than unfertilized soils). These results were consistent across grazing and liming treatments suggesting that whilst multi-nutrient additions increase plant productivity, soil C sequestration is increased by N-only additions. The positive N-only effect on soil C content was not related to changes in plant species diversity or to the functional composition of the plant community. N-only fertilized grasslands show, however, increases in total root mass and the accumulation of organic matter detritus in topsoils. Finally, soils receiving any N addition (N only or N in combination with other nutrients) were associated with high N losses. Overall, our results demonstrate that nutrient fertilization remains an important global change driver of ecosystem functioning, which can strongly affect the long-term sustainability of grassland soil ecosystems (e.g., soils ability to deliver multiple ecosystem services).
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机译:人类活动大大增加了全球许多土壤生态系统中生物活性形式的养分[例如氮(N),磷(P),钾(K),镁(Mg)]的可用性。多种营养施肥可以大大提高植物的生产力,但也可能改变土壤中碳(C)的存储量,这代表着地球上最大的有机碳库。尽管从全球变化的角度来看,这个问题很重要,但关键问题仍然在于氮的添加或氮与其他养分的结合可能会影响人为管理的土壤中的碳固存。在这里,我们在永久性草地上使用了19年的养分添加试验,以测试养分诱导的对土壤固碳的影响。我们表明,将NPKMg组合添加到永久性草地中已将土壤C的固存“限制”到与未施肥地相似的水平,而单次添加N显着增强了土壤C储量(仅N的施肥土壤平均存储11 t C ha-1超过未施肥的土壤)。这些结果在放牧和石灰处理中是一致的,这表明尽管添加多种营养素可提高植物的生产力,但仅添加氮素会增加土壤碳的固存。仅氮素对土壤碳含量的正效应与植物物种多样性的变化或植物群落的功能组成无关。但是,仅施氮的草地显示出根总质量增加以及表土中有机物碎屑的积累。最后,任何添加氮(仅氮或氮与其他养分结合)的土壤都与高氮损失有关。总体而言,我们的结果表明养分施肥仍然是生态系统功能的重要全球变化驱动力,这可能严重影响草原土壤生态系统的长期可持续性(例如土壤提供多种生态系统服务的能力)。
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