College of Resources and Environmental Engineering, Ludong
University, Yantai, Shandong Province, 264025, China
Key Laboratory of Agricultural Soil and Water Engineering in Arid
and Semiarid Areas, Ministry of Education, Northwest A & F University, Yangling, Shaanxi Province, 712100, China
Department of Soil Science, University of Saskatchewan, Saskatoon,
SK S7N 5A8, Canada
Jingjing Jin
Key Laboratory of Agricultural Soil and Water Engineering in Arid
and Semiarid Areas, Ministry of Education, Northwest A & F University, Yangling, Shaanxi Province, 712100, China
College of Resources and Environmental Engineering, Ludong
University, Yantai, Shandong Province, 264025, China
Department of Soil Science, University of Saskatchewan, Saskatoon,
SK S7N 5A8, Canada
Xiaojun Ma
Gansu Provincial Department of Water Resources, Lanzhou, Gansu
Province, 730000, China
Mingyi Wen
Key Laboratory of Agricultural Soil and Water Engineering in Arid
and Semiarid Areas, Ministry of Education, Northwest A & F University, Yangling, Shaanxi Province, 712100, China
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Evaporation led to progressively more heavy-isotope-enriched bulk soil water (BW) following the precipitation/irrigation of heavy-isotope-depleted new water but causes progressively more heavy-isotope-depleted BW following irrigation of heavy-isotope-enriched new water. The results indicated that δ2H and δ18O in evaporating water (EW) were similar to new water and differed from BW. However, the evaporative water loss calculated from BW did not differ significantly from that of EW.
Evaporation led to progressively more heavy-isotope-enriched bulk soil water (BW) following the...
