Effects of Physicochemical Properties on Soil Water Vapour Sorption Kinetics

IF 3.8 2区 农林科学 Q2 SOIL SCIENCE
Zizheng Deng, Chong Chen, Xue Song, Jianying Shang, Hu Zhou
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Abstract

Soil water vapour sorption kinetics is of great significance to understanding the soil water cycle and soil water vapour movement in arid areas. However, the differences and influencing factors of soil water vapour sorption kinetics in different adsorption processes are still not completely clear. Thus, this study aimed to investigate the soil water vapour adsorption/desorption rates (Ra/Rd) for various water activity (aw) levels and to identify the key factors affecting these rates. In this study, we determined the change of Ra and Rd with aw and the Ra and Rd during the monolayer adsorption (aw = 0.05–0.02, Ra0 and Rd0), multilayer adsorption (aw = 0.2–0.6, Ram and Rdm), and condensation (aw = 0.6–0.93, Rac and Rdc) processes for eight mineral soils with different clay contents and mineralogies using a fully-automated AquaLab Vapour Sorption Analyser in dynamic dewpoint isotherm (DDI) mode. Across the entire aw range, the Ra varied from 2.18 × 10−5 to 1.85 × 10−4 g g−1 min−1, and the Rd varied from 2.23 × 10−5 to 3.93 × 10−4 g g−1 min−1. The adsorption rate was in the order of Ra0 > Ram>Rac, and the desorption rate was in the order of Rdc>Rdm > Rd0. The ratios of adsorption and desorption rates Ra0/Rd0, Ram/Rdm, and Rac/Rdc are 2.82, 0.97, and 0.48, respectively. The monolayer adsorption rate exceeded its desorption rate, while multilayer adsorption exhibited comparable kinetics to desorption. Adsorption kinetics during capillary condensation exhibited significant retardation compared to desorption dynamics. Cation exchange capacity (CEC) and total specific surface area (SSA) were significant determinants of adsorption–desorption kinetic parameters (Ra0, Rd0, Ram, Rdm, and Rac), whereas pore volume (PV) and clay content showed no statistically significant correlation with these kinetic metrics. In contrast, clay content, external SSA, and PV emerged as key factors affecting the Rac, while CEC and total SSA exhibited negligible influence on this parameter.

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理化性质对土壤水蒸气吸附动力学的影响
土壤水蒸气吸附动力学对认识干旱区土壤水循环和土壤水蒸气运动具有重要意义。然而,不同吸附过程中土壤水蒸气吸附动力学的差异及影响因素尚不完全清楚。因此,本研究旨在研究不同水活度(aw)水平下土壤水蒸气吸附/解吸速率(Ra/Rd),并确定影响这些速率的关键因素。在本研究中,我们使用全自动AquaLab蒸汽吸附分析仪在动态露点等温线(DDI)模式下,测定了8种不同粘土含量和矿物学的矿质土在单层吸附(aw = 0.05 ~ 0.02, Ra0和Rd0)、多层吸附(aw = 0.2 ~ 0.6, Ram和Rdm)和冷凝(aw = 0.6 ~ 0.93, Rac和Rdc)过程中Ra和Rd随aw的变化,以及Ra和Rd随aw的变化。在整个光谱范围内,Ra在2.18 × 10−5到1.85 × 10−4 g g−1 min−1之间变化,Rd在2.23 × 10−5到3.93 × 10−4 g g−1 min−1之间变化。吸附速率为Ra0 >; Ram>Rac,解吸速率为Rdc>;Rdm > Rd0。吸附速率Ra0/Rd0、Ram/Rdm和Rac/Rdc分别为2.82、0.97和0.48。单层吸附速率大于脱附速率,多层吸附速率与脱附速率相当。与脱附动力学相比,毛细冷凝过程中的吸附动力学表现出明显的延迟。阳离子交换容量(CEC)和总比表面积(SSA)是吸附-解吸动力学参数(Ra0、Rd0、Ram、Rdm和Rac)的重要决定因素,而孔隙体积(PV)和粘土含量与这些动力学参数没有统计学上的显著相关性。粘土含量、外部SSA和PV是影响Rac的关键因素,而CEC和总SSA对Rac的影响可以忽略不计。
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来源期刊
European Journal of Soil Science
European Journal of Soil Science 农林科学-土壤科学
CiteScore
8.20
自引率
4.80%
发文量
117
审稿时长
5 months
期刊介绍: The EJSS is an international journal that publishes outstanding papers in soil science that advance the theoretical and mechanistic understanding of physical, chemical and biological processes and their interactions in soils acting from molecular to continental scales in natural and managed environments.
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