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Soil Thermal Properties Influenced by Perennial Biofuel and Cover Crop Management
Author(s) -
Haruna Samuel I.,
Anderson Stephen H.,
Nkongolo Nsalambi V.,
Reinbott Timothy,
Zaibon Syaharudin
Publication year - 2017
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj2016.10.0345
Subject(s) - cover crop , miscanthus , agronomy , secale , vicia villosa , environmental science , perennial plant , panicum virgatum , biofuel , bioenergy , biology , ecology
Core Ideas: Cover crops significantly increased soil organic C compared with no cover crop management. Perennial biofuel and cover crops had significantly higher volumetric heat capacity than row crop management. Under laboratory‐controlled conditions, perennial biofuel and cover crops improved soil thermal properties. Heat transport is an important factor that can influence the soil environment. The objective of this study was to determine if perennial biofuel and cover crops could alter soil thermal properties. Experimental treatments included two levels of cover crops (cover crops [CC] vs. no cover crops) [NC], collectively called row crops (RC), and two biofuel crop treatments. Cover crops used included cereal rye ( Secale cereale L.), hairy vetch ( Vicia villosa subsp. villosa ), and Austrian winter pea [ Pisum sativum subsp. arvense (L.) Asch. & Graebn]. The two biofuel treatments included perennial biofuel crops (PB): giant miscanthus ( Miscanthus × giganteus J.M. Greef & Deuter ex Hodkinson & Renvoize) and switchgrass ( Panicum virgatum L.). Soil samples were collected at 10‐cm depth increments from the soil surface to a depth of 30 cm. Soil thermal properties (thermal conductivity [ λ ], volumetric heat capacity [ C V ], thermal diffusivity [ D ]), and volumetric water content ( θ ) were determined at 0, ‐33, ‐100 and ‐300 kPa soil water matric potentials. Additionally, bulk density and soil organic C (SOC) were determined. Results showed that PB had 11% higher C V at saturation, probably because they had significantly higher θ and SOC than RC management. Cover crops had 13% higher C V at saturation probably because they had significantly higher θ and SOC than no cover crop management. Row crops had significantly higher λ and D than PB. The results from the current study imply that CC and PB can change soil thermal properties by reducing λ and D and increasing C V under laboratory conditions.