Soil temperature variations between a Typic Fragiudults and a Typic Paleudults in the Ozark Highlands of Missouri
نویسندگان
چکیده
Soil temperature measurements from a Climate Analysis Network (SCAN) monitoring site in the Ozark Highlands Major Land Resource Area (MLRA 116A) were evaluated on landscapes comprising Typic Fragiudults (Scholten series) and Paleudults (Poynor series). The five soil forming factors similarfor both soils, with major difference between adjacent soils being fragipan Scholten series. Air temperatures collected weather station of USDA-Natural Resources Conservation Service near border mesic regime udic moisture zone. mean annual observed (13.5° C) was0.5° C cooler than Poynor (14.0° C). This study showed little soiltypes January to April August December. During months May, June July, was higher (by 1.1° C, 1.4° 1.2° respectively) temperature.According this study, it is possible that no properties. Thegreatest differences air during November (5.1° for 5.3°C soil); December (5.0° 4.9° (4.5° 4.4° soil). smallestdifference month March (0° 0.3° also indicated can vary by series depending properties affecting heat transfer within pedons.
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ژورنال
عنوان ژورنال: Journal of Agriculture of The University of Puerto Rico
سال: 2022
ISSN: ['0041-994X', '2308-1759']
DOI: https://doi.org/10.46429/jaupr.v105i2.20071