Nutrient cycling and limitation in soils of higher latitude ecosystems

高纬度生态系统土壤养分循环和限制

• 批准号: RGPIN-2019-04890
• 负责人: vonSperber, Christian
• 金额: $ 1.82万
• 依托单位: McGill University
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2021
• 资助国家: 加拿大
• 起止时间: 2021-01-01 至 2022-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=737930
• 关键词: Nutrient; cycling; limitation; soils; higher

Phosphorus (P) and nitrogen (N) often limit or co-limit plant growth in terrestrial ecosystems. Many studies have suggested that the availability of these two nutrients differs during soil development. While plant growth during early stages of soil development is mostly N-limited, it becomes increasingly P-limited on older soils. Most soils in Canada are relatively young on a geological timescale, because they have developed since the last glaciation approximately 12,000 years ago. For this reason, it is generally assumed that plant growth in most Canadian ecosystems is N-limited. The combustion of fossil fuels and the volatilization of N-fertilizers have substantially increased the atmospheric deposition of N in the northern hemisphere. Many natural ecosystems in Canada might therefore have shifted from being primarily N-limited to being P-limited or P co-limited, with unknown consequences to for primary productivity, plant and microbial community structures, net ecosystem exchange of CO2 and ecosystem stability and resilience. My research program therefore aims to elucidate how a changing supply of N affects the biogeochemical cycling and availability of P in soils of non-agricultural ecosystems in higher latitudes. Both laboratory and field experiments will be carried out to answer research questions ranging from the molecular to the ecosystem scale. Field experiments will be conducted in forest and wetland ecosystems, specifically in a temperate mixed deciduous and coniferous forest on Mont Saint Hilaire, QC, in an ombrotrophic bog in Mer Bleue, ON, and in a boreal forest in the Experimental Lakes Area, ON. The effect of increasing supply of N on the bioavailability of P in soils of these ecosystems will be investigated by measuring enzyme activities, changes in concentration of geochemical soil P-pools and by quantifying atmospheric P inputs to nutrient poor organic soils. A special focus will be on the use of oxygen isotopes in phosphates to trace sources, sinks and biogeochemical processes in the environmental P-cycle. If necessary, new laboratory methods will be developed to address specific questions dealing with P-cycling in soils with high organic content, for example peatland soils and boreal forest soils. In summary, this research program will give new and fundamental insights into the cycling, limitation and fluxes of P and N in terrestrial ecosystems in Canada and elsewhere, as these ecosystems adapt to anthropogenic impacts and global change.

在陆地生态系统中，磷(P)和氮(N)常常限制或共同限制植物生长。许多研究表明，在土壤发育过程中，这两种养分的可用性是不同的。在土壤发育的早期阶段，植物生长主要受氮限制，而在较老的土壤上，植物生长越来越受磷限制。加拿大的大多数土壤在地质时间尺度上相对较年轻，因为它们是在大约12000年前的最后一次冰期之后形成的。由于这个原因，一般认为大多数加拿大生态系统中的植物生长是受n限制的。化石燃料的燃烧和氮肥的挥发大大增加了北半球大气中氮的沉积。因此，加拿大的许多自然生态系统可能已经从主要限制氮转向限制磷或共同限制磷，对初级生产力、植物和微生物群落结构、二氧化碳净生态系统交换以及生态系统稳定性和恢复力的影响未知。因此，我的研究计划旨在阐明N的变化如何影响高纬度非农业生态系统土壤中生物地球化学循环和P的有效性。将进行实验室和实地实验，以回答从分子尺度到生态系统尺度的研究问题。野外试验将在森林和湿地生态系统中进行，特别是在安大略省圣希莱尔山的温带落叶和针叶林混合林、安大略省梅尔布卢的营养型沼泽和安大略省实验湖区的北方森林中进行。通过测量酶活性、地球化学土壤磷库浓度变化和定量大气磷输入到营养贫乏的有机土壤，将研究增加氮供应对这些生态系统土壤磷生物有效性的影响。将特别侧重于利用磷酸盐中的氧同位素来追踪环境p循环中的源、汇和生物地球化学过程。如有必要，将开发新的实验室方法来处理处理高有机含量土壤中磷循环的具体问题，例如泥炭地土壤和北方森林土壤。综上所述，该研究项目将为加拿大和其他地区陆地生态系统中磷和氮的循环、限制和通量提供新的和基本的见解，因为这些生态系统适应了人为影响和全球变化。