Water source of artificial plants in the northeastern margin of Tengger Desert based on hydrogen and oxygen stable isotopes

Understanding water sources and utilization strategies is essential for the water use patterns of vegetation restoration species and achieving sustainable vegetation restoration. The water use strategies of <i>Corethrodendron scoparium</i> and <i>Calligonum mongolicum</i> were studied in the afforestation area on the northeastern edge of the Tengger Desert, to provide scientific guidance for regional vegetation restoration and stand structure adjustment. We utilize hydrogen and oxygen isotope techniques and the MixSIAR model to calculate the contribution rates of these two plant species to various potential water sources from June to October. By calculating the <i>PS</i> index, we determined the competitive relationship of <i>C. scoparium</i> and <i>C. mongolicum</i> towards different water sources. The results showed that the soil moisture content in the 0-80 cm soil layer changed significantly due to rainfall and evaporation, but stabilized with increasing depth. Shallow soil water shows enriched stable isotope composition, while the isotope of groundwater is relatively stable, and the isotope of precipitation is more enriched than that of groundwater. The main water source of <i>C. scoparium</i> and <i>C. mongolicum</i> was soil moisture. The utilization rate of 0-40 cm soil layer was 27% (<i>C.scoparium</i>) and 33% (<i>C.mongolicum</i>), and the utilization rate of 40-80 cm soil layer was 32% (<i>C.scoparium</i>) and 25% (<i>C.mongolicum</i>). The average proportional similarity index (<i>PS</i> index) between the two species was 95.67%, indicating a competitive relationship with water resources. When the surface layer (0-40) soil moisture is high (July, August), both species preferentially absorb water from this layer, and the water competition is reduced. The average <i>PS</i> index is 89%. When the surface layer (0-40) was deficient in soil moisture (June, September and October), the water competition increased, and the <i>PS</i> index was 97.83%. This study emphasized the adaptation strategies of these shrubs to arid environments and found that it provided key insights for optimizing vegetation density and species composition in desert aerial seeding areas and ensuring sustainable ecological restoration in the study area.

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Publication Details

Journal
Frontiers in Plant Science
Published
2025-05-05
DOI
https://doi.org/10.3389/fpls.2025.1523085
Citations
3
Primary Topic
Groundwater and Isotope Geochemistry
Type
article
Field-Weighted Citation Impact
4.01

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article

Water source of artificial plants in the northeastern margin of Tengger Desert based on hydrogen and oxygen stable isotopes

Guodong Tang, Meng Wu, Lei Zhang, Zhenyu Zhao et al.
3 citations
Frontiers in Plant Science
Groundwater and Isotope Geochemistry
4.01
article

Water source of artificial plants in the northeastern margin of Tengger Desert based on hydrogen and oxygen stable isotopes

Guodong Tang, Meng Wu, Lei Zhang, Zhenyu Zhao, Jinrong Li
article en
3 citations

Abstract

Understanding water sources and utilization strategies is essential for the water use patterns of vegetation restoration species and achieving sustainable vegetation restoration. The water use strategies of <i>Corethrodendron scoparium</i> and <i>Calligonum mongolicum</i> were studied in the afforestation area on the northeastern edge of the Tengger Desert, to provide scientific guidance for regional vegetation restoration and stand structure adjustment. We utilize hydrogen and oxygen isotope techniques and the MixSIAR model to calculate the contribution rates of these two plant species to various potential water sources from June to October. By calculating the <i>PS</i> index, we determined the competitive relationship of <i>C. scoparium</i> and <i>C. mongolicum</i> towards different water sources. The results showed that the soil moisture content in the 0-80 cm soil layer changed significantly due to rainfall and evaporation, but stabilized with increasing depth. Shallow soil water shows enriched stable isotope composition, while the isotope of groundwater is relatively stable, and the isotope of precipitation is more enriched than that of groundwater. The main water source of <i>C. scoparium</i> and <i>C. mongolicum</i> was soil moisture. The utilization rate of 0-40 cm soil layer was 27% (<i>C.scoparium</i>) and 33% (<i>C.mongolicum</i>), and the utilization rate of 40-80 cm soil layer was 32% (<i>C.scoparium</i>) and 25% (<i>C.mongolicum</i>). The average proportional similarity index (<i>PS</i> index) between the two species was 95.67%, indicating a competitive relationship with water resources. When the surface layer (0-40) soil moisture is high (July, August), both species preferentially absorb water from this layer, and the water competition is reduced. The average <i>PS</i> index is 89%. When the surface layer (0-40) was deficient in soil moisture (June, September and October), the water competition increased, and the <i>PS</i> index was 97.83%. This study emphasized the adaptation strategies of these shrubs to arid environments and found that it provided key insights for optimizing vegetation density and species composition in desert aerial seeding areas and ensuring sustainable ecological restoration in the study area.

Frontiers in Plant ScienceVol. 16
China Institute of Water Resources and Hydropower Research (CN), Inner Mongolia Autonomous Region Meteorological Bureau (CN), Ministry of Water Resources of the People's Republic of China (CN)
Ministry of Water Resources, China Institute of Water Resources and Hydropower Research
Openalex Percentile: Top 8%
Groundwater and Isotope Geochemistry
4.01
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