scholarly journals Determination of soil–water sorption coefficients of volatile methylsiloxanes

2014 ◽  
Vol 33 (9) ◽  
pp. 1937-1945 ◽  
Author(s):  
Gary E. Kozerski ◽  
Shihe Xu ◽  
Julie Miller ◽  
Jeremy Durham
Keyword(s):  
2021 ◽  
Vol ahead-of-print (ahead-of-print) ◽  
Author(s):  
Yan Gao ◽  
Kai Chang ◽  
Xuguang Xing ◽  
Jiaping Liang ◽  
Nian He ◽  
...  

PurposeTraditional laboratory measurements of soil water diffusivity (D) and soil water retention curve (SWRC) are always time-consuming and labor-intensive. Therefore, this paper aims to present a simple and robust test method for determining D and SWRC without reducing accuracy.Design/methodology/approachIn this study, a D model of unsaturated soil was established based on Gardner–Russo model and then a combination of Gardner–Russo model with one-dimensional horizontal absorption method to obtain n and a parameters of Gardner–Russo model. One-dimensional horizontal absorption experiments on loam, silt loam and sandy clay loam were conducted to obtain the relationships between measured infiltration rate and cumulative infiltration with wetting front distance. Based on the obtained relationships, the measured infiltration data from the one-dimensional horizontal absorption tests were used to calculate n and a parameters and further constructing D and SWRC.FindingsBoth the calculated D and SWRC inversed from the infiltration data were in good agreement with the measured ones that obtained from the traditional horizontal absorption method and the centrifuge method, respectively. Error analysis indicated that only the infiltration data are enough to reliably synchronously determine D and SWRC.Originality/valueA simple and robust method is proposed for synchronous determination of soil water diffusivity and water retention curve.


1995 ◽  
Vol 36 (3) ◽  
pp. 217-228 ◽  
Author(s):  
Nicholas M. Holden ◽  
John F. Dowd ◽  
Andrew G. Williams ◽  
David Scholefield

2012 ◽  
Vol 368 (1-2) ◽  
pp. 483-492 ◽  
Author(s):  
David M. Deery ◽  
John B. Passioura ◽  
Jason R. Condon ◽  
Asitha Katupitiya
Keyword(s):  

Author(s):  
Dominique Derome ◽  
Alessandra Patera ◽  
Ahmad Rafsanjani ◽  
Saeed Abbasion ◽  
Jan Carmeliet

Wood, due to its biological origin, has the capacity to interact with water. Sorption/desorption of moisture is accompanied with swelling/shrinkage and softening/hardening of its stiffness. The correct prediction of the behavior of wood components undergoing environmental loading or industrial process requires that the hygric, thermal and mechanical (HTM) behavior of wood are considered in a coupled manner. In addition, we propose a comprehensive framework using a fully coupled poromechanical approach, where its multiscale implementation provides the capacity to take into account, directly, the exact geometry of wood cellular structure, using computational homogenization. A hierarchical model is used to take into account the subcellular composite-like organization of the material. Such advanced modeling requires high resolution experimental data for the appropriate determination of inputs and for its validation.


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