The objective of this study is to expand our exploration of the effects of the soil environment on landmine detection by investigating the influence of soil texture and water content on surface soil temperatures above antitank mines buried at 15 cm depth and away from it. Temperature distributions in July were calculated in six soil textures for the climatic conditions of Kuwait and Sarajevo. We evaluated the temperature distributions in typical dry and wet soil profiles. The simulated temperature differences varied from .22-.63 degree Celsius in Kuwait to .16-.37 in Sarajevo. Temperature differences were - with one exception - larger in the wet than in the dry soils which suggests that soil watering may help improve thermal signatures. A major finding of this study is that the thermal signature of an anti tank mine strongly depends on the complex interaction between soil texture, water content, and geographical location. It is very difficult to predict the exact time or even the approximate hour of the appearance or nonappearance of a thermal signature. Therefore, this modeling study indicates that the use of a thermal sensor in a real mine field for instantaneous mine detection carries a high risk. On the other hand if a given area can b monitored constantly with a thermal sensor for twelve hours or longer the thermal signature will be detected if the signal to noise ratio of the mine environment allows so. Field experiments are needed to validate the results of this modeling study.
[1]
Robert Horton,et al.
Soil Heat and Water Flow With a Partial Surface Mulch
,
1987
.
[2]
Marios Sophocleous,et al.
Analysis of water and heat flow in unsaturated‐saturated porous media
,
1979
.
[3]
Omar T. Farouki,et al.
The thermal properties of soils in cold regions
,
1981
.
[4]
Jan M. H. Hendrickx,et al.
Modeling distributions of water and dielectric constants around land mines in homogeneous soils
,
1999,
Defense, Security, and Sensing.
[5]
Jan M. H. Hendrickx,et al.
Enhancing dielectric contrast between land mines and the soil environment by watering: modeling, design, and experimental results
,
2000,
Defense, Security, and Sensing.
[6]
Jan M. H. Hendrickx,et al.
MODELING TRANSIENT WATER DISTRIBUTIONS AROUND LANDMINES IN BARE SOILS
,
2001
.
[7]
H. E. Jobson.
Evaporation Into the Atmosphere: Theory, History, and Applications
,
1982
.
[8]
Marcel Fuchs,et al.
The heat flux density in a non-homogeneous bare loessial soil
,
1972
.