Abstract
A thermally insulated tensiometer was developed to investigate the water movement under frozen soils at a study site in the central part of the Tokachi Plain which is one of the largest agricultural areas of seasonally frozen soil in Japan. The above- and below-ground parts of tensiometers, which are susceptible to freezing, were housed in a thermally insulated chamber with a small internal heat source (a 5-W incandescent light bulb). The matric potentials below frozen layer were monitored using the tensiometers with other soil and meteorological parameters in the winter of 2001-2002 and 2002-2003. The data indicated that tensiometers for long-term monitoring of matric potential under frozen soil in a snow covered environment should have; (i) a sufficiently large water reservoir, (ii) the bottom half of the heated chamber buried to keep it from rising with frost heave, (iii) a relatively low-power incandescent light bulb and sufficient distance between the heated chamber and porous cups to reduce the influence of the chamber on soil temperature and water potential. Taking these into account, a new tensiometer was designed and used in the winter of 2003-2004, resulting in significantly improved data quality.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.