Soil Thermal Properties: Influence of No-Till Cover Crops

Md Ariful Haque, Seockmo Ku, Samuel I. Haruna
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Abstract

Soil thermal properties, which determines heat transport, can influence soil health parameters and crop productivity. The objective of this study was to evaluate the 2-year effects of no-till cover crops (CCs) and no-till no cover crop (NC) on soil thermal properties (thermal conductivity [λ], volumetric heat capacity [CV], and thermal diffusivity [D]). Two levels of CCs were used for this study: CC vs NC. The CCs included crimson clover (Trifolium incarnatum, L.), hairy vetch (Vicia villosa Roth.), winter peas (Lathyrus hirsutus L.), oats (Avena sativa), winter wheat (Triticum aestivum L.), triticale (Triticale hexaploide Lart.), flax (Linum usitassimum L.), and barley (Hordeum vulgare L.). Soil samples were collected at 0-10, 10-20, and 20-30 cm depths and their λ, CV, and D were measured in the laboratory. Additionally, soil organic carbon (SOC), bulk density (BD), and volumetric water content (ϴ) at saturation, -33kPa, and -100 kPa soil water pressures were measured. Results showed that BD was 18% and 14% higher under CC compared with NC management during 2021 and 2022, respectively. Furthermore, ϴ at all measured soil water pressures was slightly higher under CC compared with NC management during both years. As a result, λ and D were significantly higher under NC compared with CC management, while CV was significantly higher under CC compared with NC management, during both years and at all measured soil water pressures. Generally, soil thermal properties were directly proportional to ϴ, suggesting that ϴ may be the most important factor influencing soil thermal properties.
土壤热特性:免耕覆盖作物的影响
土壤热特性决定了热量的传输,可影响土壤健康参数和作物产量。本研究旨在评估免耕覆盖作物(CCs)和免耕无覆盖作物(NC)对土壤热特性(导热系数 [λ]、容积热容量 [CV] 和热扩散率 [D])的两年影响。本研究使用了两个级别的 CC:CC 与 NC。CCs 包括深红三叶草(Trifolium incarnatum, L.)、毛绒毛草(Vicia villosa Roth.)、冬豌豆(Lathyrus hirsutus L.)、燕麦(Avena sativa)、冬小麦(Triticum aestivum L.)、三棱麦(Triticale hexaploide Lart.)、亚麻(Linum usitassimum L.)和大麦(Hordeum vulgare L.)。在 0-10 厘米、10-20 厘米和 20-30 厘米深处采集土壤样本,并在实验室测量其 λ、CV 和 D。此外,还测量了饱和、-33 千帕和-100 千帕土壤水压下的土壤有机碳(SOC)、容重(BD)和体积含水量(ϴ)。结果表明,在 2021 年和 2022 年期间,与 NC 管理相比,CC 管理下的 BD 分别高出 18% 和 14%。此外,在所有测得的土壤水分压力下,CC 管理下的ϴ均略高于 NC 管理下的ϴ。因此,在这两年的所有测量土壤水压下,NC 管理下的λ 和 D 都明显高于 CC 管理下的λ 和 D,而 CC 管理下的 CV 则明显高于 NC 管理下的 CV。一般来说,土壤热特性与ϴ成正比,这表明ϴ可能是影响土壤热特性的最重要因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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