A framework for sourcing of evaporation between saturated and unsaturated zone in bare soil condition

被引:17
作者
Balugani, E. [1 ]
Lubczynski, M. W. [1 ]
Metselaar, K. [2 ]
机构
[1] Univ Twente, Fac Geoinformat Sci & Earth Observat ITC, Enschede, Netherlands
[2] Wageningen Univ, Soil Phys & Land Management Dept, Wageningen, Netherlands
来源
HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES | 2016年 / 61卷 / 11期
关键词
evaporation; sourcing; liquid and vapour flow; HYDRUS; ground water balance; ARID SYSTEM HYDRODYNAMICS; DESERT VADOSE ZONES; EDDY COVARIANCE; GROUND-WATER; DRY SOILS; SAP-FLOW; EVAPOTRANSPIRATION; FLUXES; VAPOR; DEUTERIUM;
D O I
10.1080/02626667.2014.966718
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Sourcing subsurface evaporation (E-ss) into groundwater (E-g) and unsaturated zone (E-u) components has received little scientific attention so far, despite its importance in water management and agriculture. We propose a novel sourcing framework, with its implementation in dedicated post-processing software called SOURCE (used along with the HYDRUS1D model), to study evaporation sourcing dynamics, define quantitatively shallow and deep water table conditions and test the applicability of water table fluctuation (WTF) and bucket methods for estimation of E-g and E-u separately.For the shallow and deep water table we propose E-g>0.95E(ss) and E-g=0 criteria, respectively. Assessment of the WTF method allowed sourcing of very small fluxes otherwise neglected by standard hydrological methods. Sourcing with SOURCE software was more accurate than the standard bucket method mainly because of greater flexibility in spatio-temporal discretization. This study emphasized the dry condition relevance of groundwater evaporation which should be analysed by applying coupled flow of heat, vapour and liquid water.
引用
收藏
页码:1981 / 1995
页数:15
相关论文
共 55 条
[1]  
Allison G. B., 1998, INT S MEM JEAN CHARL
[2]   THE DISTRIBUTION OF DEUTERIUM AND O-18 IN DRY SOILS .2. EXPERIMENTAL [J].
ALLISON, GB ;
BARNES, CJ ;
HUGHES, MW .
JOURNAL OF HYDROLOGY, 1983, 64 (1-4) :377-397
[3]  
[Anonymous], 1998, Environmental Soil Physics: Fundamentals, Applications, and Environmental Considerations
[4]  
[Anonymous], 2001, NUMERICAL PYTHON
[5]   What limits evaporation from Mediterranean oak woodlands - The supply of moisture in the soil, physiological control by plants or the demand by the atmosphere? [J].
Baldocchi, Dennis D. ;
Xu, Liukang .
ADVANCES IN WATER RESOURCES, 2007, 30 (10) :2113-2122
[6]   THE DISTRIBUTION OF DEUTERIUM AND O-18 IN DRY SOILS .1. THEORY [J].
BARNES, CJ ;
ALLISON, GB .
JOURNAL OF HYDROLOGY, 1983, 60 (1-4) :141-156
[7]  
Brooks R.J., 1964, Hydrology Paper 3, DOI DOI 10.13031/2013.40684
[8]   DESORPTION AND THE 2 STAGES OF DRYING OF NATURAL TALLGRASS PRAIRIE [J].
BRUTSAERT, W ;
CHEN, DY .
WATER RESOURCES RESEARCH, 1995, 31 (05) :1305-1313
[9]   Evapotranspiration partitioning in semiarid shrubland ecosystems: a two-site evaluation of soil moisture control on transpiration [J].
Cavanaugh, Michelle L. ;
Kurc, Shirley A. ;
Scott, Russell L. .
ECOHYDROLOGY, 2011, 4 (05) :671-681
[10]  
CHRISTOPHER P, 1982, WATER RESOUR RES, V18, P489, DOI 10.1029/WR018i003p00489