Author's guidelines
Author(s) -
Masahiro Yamashita,
Hiroyuki
Publication year - 1973
Publication title -
the forestry chronicle
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.335
H-Index - 49
eISSN - 1499-9315
pISSN - 0015-7546
DOI - 10.5558/tfc49159-4
Subject(s) - environmental science
Both evaporation rate and temperature can be estimated from δD and δ18O values of water before and after evaporation. From laboratory evaporation test results of water under uniform temperature condition, relations between evaporation rate, δD and δ18O values of water before and after evaporation were expressed at each temperature as the following equations, Y = -0.44X1 + 12.67X2 + 50.90 : 20 degrees C, Y = 0.30X1 + 1.88X2 + 41.86 : 25 degrees C, Y = -1.70X1 +11.80X2 + 7.74 : 30 degrees C, Y = -0.11X1 + 6.37X2+ 34.74 : 35 degrees C, Y = -0.71X1 + 6.82X2+ 35.11: 40 degrees C and Y = -0.17X1 + 4.94X2 +30.05 : 50 degrees C. Y is evaporation rate. X1 is δDae – δDbe – 51.3. X2 is δ18Oae δ18Obe -7.52. δDbe and δDae are δD values of water before and after evaporation. δ18Obe and δ18Oae are δ18O values of water before and after evaporation. Evaporation temperature can be also estimated from δD and δ18O values of water before and after evaporation. Relation was expressed by the equation, (δDae – δDbe – 51.3) / (δ18Oae δ18Obe -7.52) = -0.064 × temperature + 7.45. From δD and δ18O distribution map of water before and after evaporation, both evaporation rate and temperature can be also estimated.
Accelerating Research
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom
Address
John Eccles HouseRobert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom