Isotope fractionation of sandy-soil water during evaporation – an experimental study

References

• Barnes CJ, Allison GB. Tracing of water movement in the unsaturated zone using stable isotopes of hydrogen and oxygen. J Hydrol. 1988;100:143–176. doi: 10.1016/0022-1694(88)90184-9
   Web of Science ®Google Scholar
• Brooks JR, Barnard HR, Coulombe R, et al. Ecohydrologic separation of water between trees and streams in a Mediterranean climate. Nat Geosci. 2010;3:100–104. doi: 10.1038/ngeo722
   Web of Science ®Google Scholar
• Brunner P, Li HT, Kinzelbach W, et al. Extracting phreatic evaporation from remotely sensed maps of evapotranspiration. Water Resour Res. 2008;44:W08428. doi: 10.1029/2007WR006063
   Google Scholar
• DePaolo DJ, Conrad ME, Maher K, et al. Evaporation effects on oxygen and hydrogen isotopes in deep vadose zone pore fluids at Hanford, Washington. Vadose Zone J. 2004;3:220–232. doi: 10.2113/3.1.220
   Web of Science ®Google Scholar
• Gazis C, Feng X. A stable isotope study of soil water: evidence for mixing and preferential flow paths. Geoderma. 2004;119:97–111. doi: 10.1016/S0016-7061(03)00243-X
   Web of Science ®Google Scholar
• Herczeg AL, Leaney FW. Review: environmental tracers in arid-zone hydrology. Hydrol J. 2011;19:17–29.
   Google Scholar
• Izbicki JA, Radyk J, Michel RL. Water movement through a thick unsaturated zone underlying an intermittent stream in the western Mojave Desert, southern California, USA. J Hydrol. 2000;238:194–217. doi: 10.1016/S0022-1694(00)00331-0
   Web of Science ®Google Scholar
• Kendall C, Mcdonnell JJ. Isotope tracers in catchment hydrology. Amsterdam: Elsevier; 1998.
   Google Scholar
• Li FD, Song XF, Tang CY, et al. Tracing infiltration and recharge using stable isotope in Taihang Mts., North China. Environ Geol. 2007;53:687–696. doi: 10.1007/s00254-007-0683-0
   Web of Science ®Google Scholar
• Phillips FM. Environmental tracers for water movement in desert soils of the American southwest. Soil Sci Soc Am J. 1994;58:15–24. doi: 10.2136/sssaj1994.03615995005800010003x
   Web of Science ®Google Scholar
• Shurbaji ARM, Campbell AR. A study of evaporation and recharge in desert soils using environmental tracers, New Mexico, USA. Environ Geol. 1997;29:147–151. doi: 10.1007/s002540050112
   Google Scholar
• Song X, Wang S, Xiao G, et al. A study of soil water movement combining soil water potential with stable isotopes at two sites of shallow groundwater areas in the North China Plain. Hydrol Process. 2009;23:1376–1388. doi: 10.1002/hyp.7267
   Web of Science ®Google Scholar
• Dincer T, AI-Mugrin A, Zimmermann U. Study of the infiltration and recharge through sand dunes in arid zones with special reference to the stable isotopes and thermonuclear tritium. J Hydrol. 1974;23:71–109. doi: 10.1016/0022-1694(74)90025-0
   Web of Science ®Google Scholar
• Liu BL, Phillips FM, Hoines S, et al. Water movement in desert soil traced by hydrogen and oxygen isotopes, chloride, and chlorine-36, southern Arizona. J Hydrol. 1995;168:91–110. doi: 10.1016/0022-1694(94)02646-S
   Web of Science ®Google Scholar
• Knowlton RG, Phillips FM, Campbell AR. A stable-isotope investigation of vapor transport during ground-water recharge in New Mexico. Report No. 237. Las Cruces: New Mexico Water Resource Research Institute; 1989.
   Google Scholar
• Newman BD, Campbell AR, Wilcox BP. Tracer-based studies of soil water movement in semi-arid forests of New Mexico. J Hydrol. 1997;196:251–270. doi: 10.1016/S0022-1694(96)03320-3
   Web of Science ®Google Scholar
• Shurbaji AM, Phillips FM, Campbell AR, et al. Application of a numerical model for simulating water flow, isotope transport, and heat transfer in the unsaturated zone. J Hydrol. 1995;171:143–163. doi: 10.1016/0022-1694(95)02756-F
   Web of Science ®Google Scholar
• Zimmermann U, Ehhalt D, Münnich KO. Soil water movement and evapo-transpiration: changes in the isotopic composition of the water. International Atomic Energy Agency. Symposium on Isotopes in Hydrology. Proceedings; 1966 Nov 14–18; Vienna: IAEA; 1967.
   Google Scholar
• Allison GB, Barnes CJ, Hughes MW. The distribution of deuterium and oxygen-18 in dry soils: II. Experimental. J Hydrol. 1983;64:377–397. doi: 10.1016/0022-1694(83)90078-1
   Web of Science ®Google Scholar
• Araguás-Araguás L, Rozanski K, Gonfiantini R, et al. Isotope effects accompanying vacuum distillation of soil water for stable isotope analyses. J Hydrol. 1995;168:159–171. doi: 10.1016/0022-1694(94)02636-P
   Web of Science ®Google Scholar
• Walker GR, Woods PH, Allison GB. Interlaboratory comparison of methods to determine the stable isotope composition of soil water. Chem Geol. 1994;111:297–306. doi: 10.1016/0009-2541(94)90096-5
   Web of Science ®Google Scholar
• Caballero E, Jiménez de Cisneros C. Hydration properties of bentonites from Cabode Gata (SE, Spain). Isotopic study (18O/16O;2H/1H) of the hydration water. Chem Erde. 2011;71:389–395. doi: 10.1016/j.chemer.2011.03.002
   Web of Science ®Google Scholar
• De Smedt F, Wierenga PJ. Solute transfer through column of glass beads. Water Resour Res. 1984;20:225–232. doi: 10.1029/WR020i002p00225
   Web of Science ®Google Scholar
• Fialips CI, Carey JW, Vaniman DT, et al. Hydration state of zeolites, clays, and hydrated salts under present-day Martian surface conditions: can hydrous minerals account for Mars Odyssey observations of near-equatorial water-equivalent hydrogen? Icarus. 2005;178:74–83. doi: 10.1016/j.icarus.2005.04.020
   Web of Science ®Google Scholar
• Figueroa-Johnson MA, Tindall JA, Friedel M. A comparison of δ18O composition of water extracted from suction lysimeters, centrifugation, and azeotropic distillation. Water Air Soil Pollut. 2007;184:63–75. doi: 10.1007/s11270-007-9399-8
   Web of Science ®Google Scholar
• Gaudet JP, Jegat H, Vachaud G, et al. Solute transfer, with exchange between mobile and stagnant water, through unsaturated sand. Soil Sci Soc Am J. 1977;41:665–671. doi: 10.2136/sssaj1977.03615995004100040009x
   Web of Science ®Google Scholar
• Hsieh JCC, Savin SM, Kelly EF, et al. Measurement of soil-water δ18O values by direct equilibration with CO2. Geoderma. 1998;82:255–268. doi: 10.1016/S0016-7061(97)00104-3
   Web of Science ®Google Scholar
• Landon MK, Delin GN, Komor SC, et al. Comparison of the stable-isotopic composition of soil water collected from suction lysimeters, wick samplers, and cores in a sandy unsaturated zone. J Hydrol. 1999;224:45–54. doi: 10.1016/S0022-1694(99)00120-1
   Web of Science ®Google Scholar
• Playà E, Recio C, Mitchell J. Distillation of gypsum hydration water for oxygen isotopic analysis by the guanidine hydrochloride reaction method. Chem Geol. 2005;217:89–96. doi: 10.1016/j.chemgeo.2004.12.005
   Web of Science ®Google Scholar
• Sun H, Nelson M, Chen F, et al. Soil mineral structural water loss during loss on ignition analyses. Can J Soil Sci. 2009;89:603–610. doi: 10.4141/CJSS09007
   Web of Science ®Google Scholar
• Van Genuchten MT, Wierenga PJ. Mass transfer studies in sorbing porous media. I. Analytical solutions. Soil Sci Soc Am J. 1976;40:473–480. doi: 10.2136/sssaj1976.03615995004000040011x
   Web of Science ®Google Scholar
• Zheng YF, Chen JF. Stable isotope geochemistry. Beijing: Science Press in China; 2000. Chinese.
   Google Scholar
• Oerter E, Finstad K, Schaefer J, et al. Oxygen isotope fractionation effects in soil water via interaction with cations (Mg, Ca, K, Na) adsorbed to phyllosilicate clay minerals. J Hydrol. 2014;515:1–9. doi: 10.1016/j.jhydrol.2014.04.029
   Web of Science ®Google Scholar
• Wang YJ, Lu S, Ren TS, et al. Bound water content of air-dry soils measured by thermal analysis. Soil Sci Soc Am J. 2011;75:481–487. doi: 10.2136/sssaj2010.0065
   Web of Science ®Google Scholar
• Craig H, Gordon LI. Deuterium and oxygen-18 variations in the ocean and marine atmosphere. In: Tongiorgi E, editor. Stable isotopes in oceanographic studies and paleotemperatures. Proceedings; 1965; Spoleto, Italy: Consiglio Nazionale delle Ricerche, Pisa; 1965.
   Google Scholar
• Gonfiantini R. Environmental isotopes in lake studies. In: Fritz P, Fontes J-C, editors. Handbook of environmental isotope geochemistry: the terrestrial environment. Amsterdam: Elsevier; 1986. p. 113–168.
   Google Scholar
• Gat JR. Comments on stable isotope method in regional groundwater investigations. Water Resour Res. 1971;7:980–993. doi: 10.1029/WR007i004p00980
   Web of Science ®Google Scholar
• Merlivat L. Molecular diffusivities of H216O, HD16O and H218O in gases. J Chem Phys. 1978;69:2864–2871. doi: 10.1063/1.436884
   Web of Science ®Google Scholar
• Rao WB, Chen J, Tan HB, et al. Sr–Nd isotopic and REE geochemical constraints on the provenance of fine-grained sands in the Ordos deserts, north-central China. Geomorphology. 2011;132:123–138. doi: 10.1016/j.geomorph.2011.05.003
   Web of Science ®Google Scholar
• West AG, Patrickson SJ, Ehleringer JR. Water distillation times for plant and soil materials used in stable isotope analysis. Rapid Commun Mass Spectrom. 2006;20:1317–1321. doi: 10.1002/rcm.2456
   PubMed Web of Science ®Google Scholar
• Gardner CMK, Robinson D, Blyth K, et al. Soil water content. In: Smith KA, Mullins CE, editors. Soil and environmental analysis: physical methods. New York: Marcel Dekker; 2001. p. 1–64.
   Google Scholar
• Logsdon SD, Laird D. Electrical conductivity spectra of smectites as influenced by saturating cation and humidity. Clay Clay Miner. 2004;52:411–420. doi: 10.1346/CCMN.2004.0520402
   Web of Science ®Google Scholar
• Mitchell JK, Soga K. Fundamentals of soil behavior. Hoboken, NJ: John Wiley & Sons; 2005.
   Google Scholar
• Kurc S, Small E. Dynamics of evapotranspiration in semiarid grassland and shrubland ecosystems during the summer monsoon season, central New Mexico. Water Resour Res. 2004;40:W09305. doi: 10.1029/2004WR003068
   Web of Science ®Google Scholar
• Craig H. Isotopic variation in meteoric waters. Science. 1961;133:1702–1703. doi: 10.1126/science.133.3465.1702
   PubMed Web of Science ®Google Scholar