Article ID Journal Published Year Pages File Type
5744358 Journal of Arid Environments 2017 12 Pages PDF
Abstract

•Distribution of grassland types was mapped, including their corresponding P inputs and outputs.•The overall net balance of P was quantified in different grassland types.•Natural grasslands had a small range of P balance (between −2.01 and 1.2 kg P ha−1).•Managed grasslands had a wide range of P balance (between −42 and 126 kg P ha−1).

Grasslands, accounting for one third of the world terrestrial land surface, are important in determining phosphorus (P) cycle at a global scale. Understanding the impacts of management on P inputs and outputs in grassland ecosystem is crucial for environmental management since a large amount of P is transported through rivers and groundwater and detained by the sea reservoir every year. To better understand P cycle in global grasslands, we mapped the distribution of different grassland types around the world and calculated the corresponding P inputs and outputs for each grassland type using data from literature. The distribution map of P input and output revealed a non-equilibrium condition in many grassland ecosystems, with: (i) a greater extent of input than output in most managed grasslands, but (ii) a more balanced amount between input and output in the majority of natural grasslands. Based on the mass balance between P input and output, we developed a framework to achieve sustainable P management in grasslands and discussed the measures targeting a more balanced P budget. Greater challenge is usually found in heavily-managed than natural grasslands to establish the optimum amount of P for grass and livestock production while minimizing the adverse impacts on surface waters. This study provided a comprehensive assessment of P budget in global grasslands and such information will be critical in determining the appropriate P management measures for various grassland types across the globe.

Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
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