Department of Ecology, Evolution and Behavior, University of Minnesota, Saint Paul, MN 55108, USA.
Glob Chang Biol. 2013 Apr;19(4):1249-61. doi: 10.1111/gcb.12096. Epub 2013 Jan 10.
The effects of global environmental changes on soil nitrogen (N) pools and fluxes have consequences for ecosystem functions such as plant productivity and N retention. In a 13-year grassland experiment, we evaluated how elevated atmospheric carbon dioxide (CO2 ), N fertilization, and plant species richness alter soil N cycling. We focused on soil inorganic N pools, including ammonium and nitrate, and two N fluxes, net N mineralization and net nitrification. In contrast with existing hypotheses, such as progressive N limitation, and with observations from other, often shorter, studies, elevated CO2 had relatively static and small, or insignificant, effects on soil inorganic N pools and fluxes. Nitrogen fertilization had inconsistent effects on soil N transformations, but increased soil nitrate and ammonium concentrations. Plant species richness had increasingly positive effects on soil N transformations over time, likely because in diverse subplots the concentrations of N in roots increased over time. Species richness also had increasingly positive effects on concentrations of ammonium in soil, perhaps because more carbon accumulated in soils of diverse subplots, providing exchange sites for ammonium. By contrast, subplots planted with 16 species had lower soil nitrate concentrations than less diverse subplots, especially when fertilized, probably due to greater N uptake capacity of subplots with 16 species. Monocultures of different plant functional types had distinct effects on N transformations and nitrate concentrations, such that not all monocultures differed from diverse subplots in the same manner. The first few years of data would not have adequately forecast the effects of N fertilization and diversity on soil N cycling in later years; therefore, the dearth of long-term manipulations of plant species richness and N inputs is a hindrance to forecasting the state of the soil N cycle and ecosystem functions in extant plant communities.
全球环境变化对土壤氮(N)库和通量的影响会影响到生态系统功能,如植物生产力和 N 保留。在一项为期 13 年的草地实验中,我们评估了大气二氧化碳(CO2)升高、N 施肥和植物物种丰富度如何改变土壤 N 循环。我们专注于土壤无机 N 库,包括铵和硝酸盐,以及两个 N 通量,净 N 矿化和净硝化。与现有假说(如渐进性 N 限制)以及其他(通常较短)研究的观察结果相反,大气 CO2 对土壤无机 N 库和通量的影响相对稳定且较小,或者没有显著影响。N 施肥对土壤 N 转化的影响不一致,但增加了土壤硝酸盐和铵的浓度。随着时间的推移,植物物种丰富度对土壤 N 转化的影响越来越积极,这可能是因为在不同的子小区中,根中的 N 浓度随着时间的推移而增加。物种丰富度也对土壤中铵的浓度产生越来越积极的影响,这可能是因为不同子小区中的碳积累越来越多,为铵提供了交换位点。相比之下,种植 16 种植物的子小区的土壤硝酸盐浓度低于物种多样性较低的子小区,尤其是在施肥的情况下,这可能是因为种植 16 种植物的子小区具有更大的 N 吸收能力。不同植物功能类型的单一种植对 N 转化和硝酸盐浓度有明显的影响,因此并非所有单一种植都以相同的方式与多种子小区不同。前几年的数据不足以预测 N 施肥和多样性对后期土壤 N 循环的影响;因此,缺乏对植物物种丰富度和 N 输入的长期操纵是预测现存植物群落土壤 N 循环和生态系统功能状态的障碍。