Using stable isotopes to determine dew formation from atmospheric water vapor in soils in semiarid regions

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• 作者：Qianlin Zhu ; Zhenbo Jiang
• 关键词：Dew formation ; Natural stable isotope ; Deuterium ; Oxygen ; Water cycle
• 刊名：Arabian Journal of Geosciences
• 出版年：2016
• 出版时间：January 2016
• 年：2016
• 卷：9
• 期：1
• 全文大小：967 KB
• 参考文献：Acker K, Beysens D, M枚ller D (2008) Nitrite in dew, fog, cloud and rain water: an indicator for heterogeneous processes on surfaces. Atmos Res 87:200鈥?12CrossRef
  Agam N, Berliner PR (2006) Dew formation and water vapor adsorption in semi-arid environments-A review. J Arid Environ 65:572鈥?90CrossRef
  Allison GB (1982) The relationship between 18O and deuterium in water in sand columns undergoing evaporation. J Hydrol 55:163鈥?69CrossRef
  Araguas-Araguas L, Froehlich K, Rozanski K (2000) Deuterium and oxygen-18 isotope composition of precipitation and atmospheric moisture. Hydrol Process 14:1341鈥?355CrossRef
  Barnes CJ, Allison GB (1988) Tracing of water movement in the unsaturated zone using stable isotopes of hydrogen and oxygen. J Hydrol 100:143鈥?76CrossRef
  Barnes CJ, Allisson GB (1983) Distribution of deuterium and 18O in dry soils 1: theory. J Hydrol 60:141鈥?56CrossRef
  Beysens D (1995) The formation of dew. Atmos Res 39:215鈥?37CrossRef
  Beysens D, Ohayon C, Muselli M, Clus O (2006) Chemical and biological characteristics of dew and rain water in an urban coastal area (Bordeaux, France). Atmos Environ 40:3710鈥?723CrossRef
  Chiwa M, Oshiro N, Miyake T, Nakatani N, Kimura N, Yuhara T, Hashimoto N, Sakugawa H (2003) Dry deposition washoff and dew on the surfaces of pine foliage on the urban- and mountain-facing sides of Mt. Gokurakuji, western Japan. Atmos Environ 37:327鈥?37CrossRef
  Craig H (1961) Isotopic variations in meteoric waters. Science 133:1702鈥?703CrossRef
  Cui J, An SQ, Wang ZS, Fang CM, Liu YH, Yang HB, Xu Z, Liu SR (2009) Using deuterium excess to determine the sources of high-altitude precipitation: implications in hydrological relations between sub-alpine forests and alpine meadows. J Hydrol 373:24鈥?3CrossRef
  Danalatos NG, Kosmas CS, Moustakas NC, Yassoglou N (1995) Rock fragments IL their impact on soil physical properties and biomass production under Mediterranean conditions. Soil Use Manage 11:121鈥?26CrossRef
  Dawson TE, Ehleringer JR (1991) Streamside trees that do not use stream water. Nature 350:335鈥?37CrossRef
  de Jong C (2005) The contribution of condensation to the water cycle under high-mountain conditions. Hydrol Process 19:121鈥?26
  Deb SK, Shukla MK, Sharma P, Mexal JG (2011) Coupled liquid water, water vapor, and heat transport simulations in an unsaturated zone of a sandy loam field. Soil Sci 176:387鈥?98CrossRef
  Fontes JC, Gonfiantini R (1967) Comportement isotopique au cours de l鈥檈vaporation de deux bassins sahariens. Earth Planet Sci Lett 3:258鈥?66CrossRef
  Foster JR, Pribush RA, Carter BH (1990) The chemistry of dews and frosts in indianapolis, Indiana. Atmospheric Environment. Part A. General Topics 24:2229鈥?236CrossRef
  Guo ZY, Han SP (2002) Experimental study on the condensation water in arid, Northwestern China. Adv Water Sci 13:623鈥?28 (in Chinese)
  Herczeg A, Leaney FW (2011) Review: environmental tracers in arid-zone hydrology. Hydrogeology J 19:17鈥?9CrossRef
  Institute of Hydrogeology and Engineering Geology, Chinese Ministry of Geology and Mineral Resources (1989) Background values of the precipitation stable isotopes in China. Invest Sci Technol 6:6鈥?2 (in Chinese)
  Jacobs AFG, Heusinkveld BG, Berkowicz SM (1999) Dew deposition and drying in desert system: a simple simulation model. J Arid Environ 42:211鈥?22CrossRef
  Jacobs AFG, Heusinkveld BG, Berkowicz SM (2002) A simple model for potential dewfall in an arid region. Atmos Res 64:285鈥?95CrossRef
  Jiries A (2001) Chemical composition of dew in Amman, Jordan. Atmos Res 57:261鈥?68CrossRef
  Kawashima H, Kurahashi T (2011) Inorganic ion and nitrogen isotopic compositions of atmospheric aerosols at Yurihonjo, Japan: implications for nitrogen sources. Atmos Environ 45:6309鈥?316CrossRef
  Kidron GJ, Starinsky A (2012) Chemical composition of dew and rain in an extreme desert (Negev): cobbles serve as sink for nutrients. J Hydrology 420鈥?21:284鈥?91CrossRef
  Kosmas C, Danalatos NG, Poesen J, Van-Wesemael B (1998) The effect of water vapour adsorption on soil moisture content under Mediterranean climatic conditions. Agi Water Manage 36:157鈥?68CrossRef
  Kosmas C, Marathianou M, Gerontidis S, Detsis V, Tsara M, Poesen J (2001) Parameters affecting water vapor adsorption by the soil under semi-arid climatic conditions. Agric Water Manage 48:61鈥?8CrossRef
  Lakhani A, Parmar R, Prakash S (2012) Chemical composition of dew resulting from radiative cooling at a semi-arid site in Agra, India. Pure Appl Geophys 169:859鈥?71CrossRef
  Leaney FW, Smettem KRJ, Chittleborough DJ (1993) Estimating the contribution of preferential flow to subsurface runoff from a hillslope using deuterium and chloride. J Hydrol 147:83鈥?03CrossRef
  Lee KS, Kim JM, Lee DR, Kim Y, Lee D (2007) Analysis of water movement through an unsaturated soil zone in Jeju Island, Korea using stable oxygen and hydrogen isotopes. J Hydrol 345:199鈥?11CrossRef
  Lekouch I, Mileta M, Muselli M, Milimouk-Melnytchouk I, 艩ojat V, Kabbachi B, Beysens D (2010) Comparative chemical analysis of dew and rain water. Atmos Res 95:224鈥?34CrossRef
  Li Y, Shao M (2006) Effects of rainfall intensity on rainfall infiltration and redistribution in soil on loess slope land. Chin J Appl Ecol 17:2271鈥?276
  Lin R, Wei K (2006) Tritium profiles of pore water in the Chinese loess unsaturated zone: implications for estimation of groundwater recharge. J Hydrol 328:192鈥?99CrossRef
  Liu BL, Phillips F, Hoines S, Cpmpbell AR, Sharma P (1995) Water movement in desert soil traced by hydrogen and oxygen isotopes, chloride and chlorine-36, southern Arizona. J Hydrol 168:91鈥?10CrossRef
  Ninari N, Berliner PR (2002) The role of dew in the water and heat balance of bare loess soil in the Negev Desert: quantifying the actual dew deposition on the soil surface. Atmos Res 64:323鈥?34CrossRef
  Porte-Agel F, Parlange MB, Cahill AT, Gruber A (2000) Mixture of time scales in evaporation: desorption and self-similarity of energy fluxes. Agron J 92:832鈥?36CrossRef
  Qin J, Wang KF, Zhan WJ (1993) A study on the coagulation water in the sandy soil and its role in water balance. Arid Zone Res. 10: 1-9 (in Chinese)
  Rubio MA, Lissi E, Villena G (2002) Nitrite in rain and dew in Santiago city, Chile. Its possible impact on the early morning start of the photochemical smog. Atmos Environ 36:293鈥?97CrossRef
  Scholl M, Eugster W, Burkard R (2010) Understanding the role of fog in forest hydrology:stable isotopes as tools for determining input and partitioning of cloud water in montane forests. Hydrol Process 35:353鈥?66
  Shurbaji ARM, Phillips FM, Campbell AR, Knowltonb RG (1995) Application of a numerical model for simulation water flow, isotopetransport, and heat transfer in the unsaturated zone. J Hydrol 171:143鈥?63CrossRef
  Singh SP, Khare P, Kumari KM, Srivastava SS (2006) Chemical characterization of dew at a regional representative site of North-Central India. Atmos Res 80:239鈥?49CrossRef
  Suleiman AA, Ritchie JT (2003) Modeling soil water redistribution during second-stage evaporation. Soil Sci Soc Am J 67:377鈥?86CrossRef
  Victoria RL, Martinelli LA, Mortatti J, Filchey J (1991) Mechanisms of water recycling in the Amazon Basin: isotopic insights. Ambio 20:384鈥?87
  White JWC, Gedzelman SD (1984) The isotopic composition of atmospheric water vapor and the concurrent meteorological conditions. J Geophys Res 89:4937鈥?939CrossRef
  Yanful EK, Mousavi SM (2003) Estimating falling rate evaporation from finite soil columns. Sci Total Environ 313:141鈥?52CrossRef
  Yatagai A (2008) The isotopic composition of water vapor and the concurrent meteorological conditions around the northeast part of the Tibetan Plateau. AMS 13th Conference on Mountain Meteorology Whistler, British Columbia, Canada
  Yin CL, Yao TD, Tian LD, Liu DN, Yu WS, Qu DM (2008) Temporal variations of 未18O of atmospheric water vapor at Delingha. Sci China Ser D-Earth Sci 51:966鈥?75CrossRef
  Yu WS, Yao TD, Tian LD (2005) Isotopic composition of atmospheric water vapor before and after the monsoon鈥檚 end in the Nagqu River Basin. Chinese Sci Bull 50:2755鈥?760CrossRef
  Zeng YJ, Wan L, Wang XS, Cao WB (2006) An experimental study of day and night trends of soil temperature and moisture in the shallow unsaturated zone. Earth Sci Front 13:52鈥?7 (in Chinese)
  
• 作者单位：Qianlin Zhu (1)
  Zhenbo Jiang (2)
  
  1. Low Carbon Energy Institute, China University of Mining and Technology, Xuzhou, 221008, China
  2. Faculty of Engineering, Kyushu University, Fukuoka, 819-03954, Japan
  
• 刊物类别：Earth and Environmental Science
• 出版者：Springer Berlin Heidelberg
• ISSN：1866-7538

文摘

Moisture sources for dew formation in soils can be classified into soil water and atmospheric water vapor. Discriminating respective contribution of the two moisture sources is important for knowledge of water balance valuation. Stable 2H and 18O of atmospheric water vapor are temporal variation; thus, they may be different to that in soil water, which makes it feasible to discriminate moisture sources between soil water and atmospheric water vapor. In this paper, we took soil samples in the semiarid northern Chinese Loess Plateau and extracted the soil water using the high-temperature vacuum distillation method. Stable isotope profiles and 未D-未18O slopes of the soil water showed that the dew condensed from atmospheric water vapor occurred mainly in the upper 20 cm of the soil layer. The atmospheric water vapor hardly influenced the soil water at 30-cm depth and the deeper soil layer. The significantly low deuterium excess of the soil water at the depth of 10 and 20 cm indicated that the dew in the soil underwent intensive evaporation after the dew formation. Keywords Dew formation Natural stable isotope Deuterium Oxygen Water cycle