Measurement of evaporation on bare soil and estimating surface resistance

被引:54
作者
Aluwihare, S [1 ]
Watanabe, K
机构
[1] Open Univ Sri Lanka, Fac Engn, Dept Civil Engn, Nawala, Sri Lanka
[2] Saitama Univ, Geosphere Res Inst, Saitama 3388570, Japan
来源
JOURNAL OF ENVIRONMENTAL ENGINEERING-ASCE | 2003年 / 129卷 / 12期
关键词
evaporation; measurement; soil water; soil resistance;
D O I
10.1061/(ASCE)0733-9372(2003)129:12(1157)
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A new evaporation measuring device incorporating an evaporation chamber has been developed and checked for its accuracy. This device is unique that it uses a chamber that is completely open at one end and thereby minimizes the effect of the chamber on the natural profiles of temperature, humidity, and turbulence. It was used in estimating a newly formulated surface resistance to bare soil evaporation under dry topsoil conditions. A simple energy balance model incorporating the depth of evaporating surface, blended with a new approach for describing surface resistance was developed and successfully tested with a limited set of data obtained from a simple experiment, assuming ideal conditions. In addition to the newly formulated surface resistance, the depth of the dry soil layer was also estimated and was relatively comparable with measured value. The newly formulated surface resistance was found to be insignificant compared to the resistance imposed by the dry soil layer. The total surface resistance was modeled as a power function of soil moisture in the top 0-1 cm of soil, while the newly formulated resistance did not show any relation with the soil moisture.
引用
收藏
页码:1157 / 1168
页数:12
相关论文
共 33 条
[1]   MEASURING WATER EXCHANGE BETWEEN SOIL AND ATMOSPHERE WITH TDR-MICROLYSIMETRY [J].
BAKER, JM ;
SPAANS, EJA .
SOIL SCIENCE, 1994, 158 (01) :22-30
[2]  
BRUTSAERT H, 1982, EVAPORATION ATMOSPHE
[3]   A RESISTANCE PARAMETER FOR BARE-SOIL EVAPORATION MODELS [J].
CAMILLO, PJ ;
GURNEY, RJ .
SOIL SCIENCE, 1986, 141 (02) :95-105
[4]  
CAMPBELL GS, 1985, SOIL PHYSICS BASIC T
[5]   SIGNIFICANCE OF SOIL SURFACE MOISTURE WITH RESPECT TO DAILY BARE SOIL EVAPORATION [J].
CHANZY, A ;
BRUCKLER, L .
WATER RESOURCES RESEARCH, 1993, 29 (04) :1113-1125
[6]   A 4-LAYER MODEL FOR THE HEAT-BUDGET OF HOMOGENEOUS LAND SURFACES [J].
CHOUDHURY, BJ ;
MONTEITH, JL .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1988, 114 (480) :373-398
[7]   USE OF MICROLYSIMETERS TO MEASURE EVAPORATION FROM SANDY SOILS [J].
DAAMEN, CC ;
SIMMONDS, LP ;
WALLACE, JS ;
LARYEA, KB ;
SIVAKUMAR, MVK .
AGRICULTURAL AND FOREST METEOROLOGY, 1993, 65 (3-4) :159-173
[8]   Measurement of evaporation from bare soil and its estimation using surface resistance [J].
Daamen, CC ;
Simmonds, LP .
WATER RESOURCES RESEARCH, 1996, 32 (05) :1393-1402
[9]   AERODYNAMIC AND SURFACE RESISTANCES AFFECTING ENERGY-TRANSPORT IN A SPARSE CROP [J].
HAM, JM ;
HEILMAN, JL .
AGRICULTURAL AND FOREST METEOROLOGY, 1991, 53 (04) :267-284
[10]  
HILLEL D, 1971, SOIL WATER PHYSICAL