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Freeze-thaw process induced by increased precipitation affects root growth of alpine steppe on the Tibetan Plateau
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...
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Published in: | Journal of mountain science 2023-10, Vol.20 (10), p.3010-3017 |
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Main Authors: | , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites |
Online Access: | Get full text |
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Summary: | 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. |
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ISSN: | 1672-6316 1993-0321 1008-2786 |
DOI: | 10.1007/s11629-023-8010-0 |