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Decoupling of soil nutrient cycles as a function of

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TLDR
In this paper, the authors evaluate how aridity affects the balance between carbon (C), nitrogen (N) and phosphorus (P) in soils collected from 224 dryland sites from all continents except Antarctica and find a negative effect of aridity on the concentration of soil organic C and total N, but a positive effect on inorganic P.
Abstract
The biogeochemical cycles of carbon (C), nitrogen (N) and phosphorus (P) are interlinked by primary production, respiration and decomposition in terrestrial ecosystems. It has been suggested that the C, N and P cycles could become uncoupled under rapid climate change because of the different degrees of control exerted on the supply of these elements by biological and geochemical processes. Climatic controls on biogeochemical cycles are particularly relevant in arid, semi-arid and dry sub-humid ecosystems (drylands) because their biological activity is mainly driven by water availability. The increase in aridity predicted for the twenty-first century in many drylands worldwide may therefore threaten the balance between these cycles, differentially affecting the availability of essential nutrients. Here we evaluate how aridity affects the balance between C, N and P in soils collected from 224 dryland sites from all continents except Antarctica. We find a negative effect of aridity on the concentration of soil organic C and total N, but a positive effect on the concentration of inorganic P. Aridity is negatively related to plant cover, which may favour the dominance of physical processes such as rock weathering, a major source of P to ecosystems, over biological processes that provide more C and N, such as litter decomposition. Our findings suggest that any predicted increase in aridity with climate change will probably reduce the concentrations of N and C in global drylands, but increase that of P. These changes would uncouple the C, N and P cycles in drylands and could negatively affect the provision of key services provided by these ecosystems.

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Citations
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DissertationDOI

Exploring the possibilities of parsimonious nitrogen modelling in different ecosystems

TL;DR: In this paper, two parsimonious nitrogen models have been developed and implemented in two different data availability scenarios, one in a semi-arid natural forest ecosystem and the other in an anthropogenic agricultural ecosystem.
Dissertation

Modelling of the topsoil organic carbon content by analysing the potential of spectroscopic techniques for digital soil mapping

TL;DR: In this article, the authors explored the capacity of spectroscopy for map soil organic carbon content at regional scale using topsoil samples from Galicia (NW-Spain) and developed a spatially non-stationary approach that allows mapping soil organic content and also identifying the factors more relevant for its accumulation in Europe.
References
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Journal ArticleDOI

Soil Phosphorus Modeling for Modern Agriculture Requires Balance of Science and Practicality: A Perspective.

TL;DR: A framework for interdisciplinary collaboration is needed to acquire suitable datasets, continually assess the need for model adjustment, and provide flexibility for progression of scientific theory to advance P management for increased P use efficiency.
Journal ArticleDOI

Low molecular weight organic acids regulate soil phosphorus availability in the soils of subalpine forests, eastern Tibetan Plateau

TL;DR: In this article, low molecular weight organic acids (LMWOAs) were analyzed in bulk and rhizosphere soils of Abie fabri dominated forests across four altitudes (2800-3500m) on Gongga Mountain, eastern Tibetan Plateau, to delineate the effects of LMWOA on the availability of soil P in response to the root exudates and altitude differentiation.
Journal ArticleDOI

Soil nitrogen response to shrub encroachment in a degrading semi-arid grassland

TL;DR: In this article, the authors quantified how the distribution and speciation of soil nitrogen, as well as rates of free-living biochemical nitrogen fixation, changed along a gradient of increasing mesquite(Prosopis velutina Woot.) cover in a semi-arid grassland of the southwestern US.
Journal ArticleDOI

Determining Land Management Zones Using Pedo-Geomorphological Factors in Potential Degraded Regions to Achieve Land Degradation Neutrality

TL;DR: In this article, a pedo-geomorphological approach using soil texture, land elevation and flow vector aspects is presented to distinguish different management zones and to discretize soil micronutrients.
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