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Data from: N balance and cycling of Inner Mongolia typical steppe - a comprehensive case study of grazing effects

Citation

Giese, Marcus et al. (2013), Data from: N balance and cycling of Inner Mongolia typical steppe - a comprehensive case study of grazing effects, Dryad, Dataset, https://doi.org/10.5061/dryad.s903c

Abstract

Increasing grazing pressure and climate change affect nitrogen (N) dynamics of grassland ecosystems in the Eurasian Steppe belt with unclear consequences for future delivery of essential services such as forage production, C sequestration, and diversity conservation. The identification of key processes responsive to grazing is crucial to optimize grassland management. In this comprehensive case study of a Chinese typical steppe, we present an in-depth analysis of grazing effects on N dynamics including the balance of N gains and losses, and N cycling. N pools and fluxes simultaneously quantified on three grassland sites of different long-term grazing intensities. Dust deposition, wind erosion, and wet deposition were predominant but most variable processes contributing to N losses and gains. Heavy grazing increased the risk of N losses by wind erosion. Haymaking and sheep excrements export to folds during night time keeping were important pathways of N losses from grassland sites. Compared to these fluxes, gaseous N losses (N2O, NO, N2 and NH3), and N losses via export of sheep live weight and wool were of minor relevance. Our N balance calculation indicated mean annual net N losses of 0.9 ({plus minus}0.8) g N m-2 at the heavily grazed site, whereas the long-term ungrazed site was an N sink receiving mean annual inputs of 1.8 ({plus minus}1.1) g N m-2, mainly due to dust deposition. Heavy grazing reduced pool sizes of both topsoil organic N, and above- and belowground biomass and N fluxes with regard to plant N uptake, decomposition, gross microbial N turnover, and immobilization. Most N-related processes were more intensive in seasons of higher water availability indicating complex interactions between land use intensity and climate variability. The projected increase of atmospheric N depositions and changes in rainfall pattern superimposed by land use change will likely affect N sink-source pathways and N flux dynamics, indicating high potential impact on grassland ecosystem functions. Land use practices will be increasingly important for the management of N dynamics in Chinese typical steppe and, therefore, must be considered as key component to maintain, restore or optimize ecosystem services.

Usage Notes

Location

Inner Mongolia
China