西班牙中部土壤和基岩热机制的热动力和水文驱动因素

IF 5.8 2区 农林科学 Q1 SOIL SCIENCE Soil Pub Date : 2024-01-10 DOI:10.5194/soil-10-1-2024
Félix García-Pereira, Jesús Fidel González-Rouco, Thomas Schmid, Camilo Melo-Aguilar, Cristina Vegas-Cañas, Norman Julius Steinert, Pedro José Roldán-Gómez, Francisco José Cuesta-Valero, Almudena García-García, Hugo Beltrami, Philipp de Vrese
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引用次数: 0

摘要

摘要利用瓜达拉马监测网(GuMNet)的四个深层(20 米)监测剖面和西班牙气象局(Agencia Estatal de Meteorología, AEMET)的两个浅层剖面(1 米)的地下和地表温度数据,对西班牙中部瓜达拉马山脉的土壤和基岩热结构进行了评估,时间跨度分别为 2015-2021 年和 1989-2018 年。对空气和地表温度耦合的评估表明,积雪覆盖造成的土壤隔热是季节性解耦的主要原因,尤其是在高海拔地区的冬季。根据年周期随深度变化的振幅衰减和相位偏移得出的表观热扩散值,通过假设热传导机制来描述地下温度传播的特征。这种方法还可进一步扩展到考虑频谱域中所有谐波的衰减,从而分析近地表土壤在短时标的高频变化所产生的热扩散率。在深层剖面上,表观热扩散率为 1 至 1.3×10-6 m2 s-1,与瓜达拉马山脉主要基岩成分片麻岩和花岗岩的数值一致。然而,在靠近地表的土层中,热扩散率较低,且更加不均匀(0.4-0.8×10-6 m2 s-1)。在 4-8 米深的土壤-岩石过渡层,热扩散率随深度的增加而增加。这些结果有助于了解土壤热力学与其他土壤特性的关系。光谱法的结果表明,近表层热扩散率的变化与土壤含水量的变化有关,这使其成为从土壤温度数据中获取有关土壤干旱和水资源可用性信息的潜在工具。
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Thermodynamic and hydrological drivers of the soil and bedrock thermal regimes in central Spain
Abstract. An assessment of the soil and bedrock thermal structure of the Sierra de Guadarrama, in central Spain, is provided using subsurface and ground surface temperature data coming from four deep (20 m) monitoring profiles belonging to the Guadarrama Monitoring Network (GuMNet) and two shallow profiles (1 m) from the Spanish Meteorology Service (Agencia Estatal de Meteorología, AEMET) covering the time spans of 2015–2021 and 1989–2018, respectively. An evaluation of air and ground surface temperature coupling showed that soil insulation due to snow cover is the main source of seasonal decoupling, being especially relevant in winter at high-altitude sites. Temperature propagation in the subsurface was characterized by assuming a heat conductive regime by considering apparent thermal diffusivity values derived from the amplitude attenuation and phase shift of the annual cycle with depth. This methodology was further extended to consider the attenuation of all harmonics in the spectral domain, which allowed for analysis of thermal diffusivity from high-frequency changes in the soil near the surface at short timescales. For the deep profiles, the apparent thermal diffusivity ranges from 1 to 1.3×10-6 m2 s−1, which is consistent with values for gneiss and granite, the major bedrock components in the Sierra de Guadarrama. However, thermal diffusivity is lower and more heterogeneous in the soil layers close to the surface (0.4–0.8×10-6 m2 s−1). An increase in diffusivity with depth was observed that was generally larger in the soil–bedrock transition at 4–8 m depth. The outcomes are relevant for the understanding of soil thermodynamics in relation to other soil properties. Results with the spectral method suggest that changes in near-surface thermal diffusivity are related to changes in soil moisture content, which makes it a potential tool to gain information about soil drought and water resource availability from soil temperature data.
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来源期刊
Soil
Soil Agricultural and Biological Sciences-Soil Science
CiteScore
10.80
自引率
2.90%
发文量
44
审稿时长
30 weeks
期刊介绍: SOIL is an international scientific journal dedicated to the publication and discussion of high-quality research in the field of soil system sciences. SOIL is at the interface between the atmosphere, lithosphere, hydrosphere, and biosphere. SOIL publishes scientific research that contributes to understanding the soil system and its interaction with humans and the entire Earth system. The scope of the journal includes all topics that fall within the study of soil science as a discipline, with an emphasis on studies that integrate soil science with other sciences (hydrology, agronomy, socio-economics, health sciences, atmospheric sciences, etc.).
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