Abstract
The response of vegetation productivity to precipitation is becoming a worldwide concern. Most reports on responses of vegetation to precipitation trends are based on the growth season. In the soil freeze/thaw process, the soil water phase and heat transport change can affect root growth, especially during the thawing process in early spring. A field experiment with increased precipitation (control, increased 25% and increased 50%) was conducted to measure the effects of soil water in early spring on above- and below-ground productivity in an alpine steppe over two growing seasons from June 2017 to September 2018. The increased 50% treatment significantly increased the soil moisture at the 10 cm depth, there was no difference in soil moisture between the increased 25% treatment and the control in the growing season, which was not consistent in the freeze/thaw process. Increased soil moisture during the non-growing season retarded root growth. Increased precipitation in the freezing-thawing period can partially offset the difference between the control and increased precipitation plots in both above- and below-ground biomass.
Data Availability Statement: Data supporting this research article are available from the corresponding author on request.
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Acknowledgments
This research was funded by the Second Tibetan Plateau Scientific Exploration, the Strategic Priority Research Program of Chinese Academy of Sciences, and the National Natural Science Foundation, grant number 2019QZKK0404, XDA20020401, 41977284 and by the Doctoral Science Foundation of Henan Polytechnic University (B2019-019).
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WANG Xiao-dan and QIN Xiao-jing: Conceptualization; QIN Xiao-jing: Methodology, software, validation, formal analysis, investigation, resources, data curation, writing—original draft preparation; HONG Jiang-tao: Writing—review and editing; NIE Xiao-jun: Visualization, supervision, project administration; WANG Xiao-dan: funding acquisition. All authors have read and agreed to the published version of the manuscript.
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Conflicts of Interest: WANG Xiao-dan is a scientific editor of Journal of Mountain Science. He was not involved in the peer-review or handling of the manuscript. The authors have no other competing interests to disclose.
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Qin, Xj., Nie, Xj., Wang, Xd. et al. Freeze-thaw process induced by increased precipitation affects root growth of alpine steppe on the Tibetan Plateau. J. Mt. Sci. 20, 3010–3017 (2023). https://doi.org/10.1007/s11629-023-8010-0
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DOI: https://doi.org/10.1007/s11629-023-8010-0