Research Article

Soil moisture adsorption capacity and specific surface area in relation to water vapor pressure in arid and tropical soils

Volume: 8 Number: 4 October 1, 2019
EN

Soil moisture adsorption capacity and specific surface area in relation to water vapor pressure in arid and tropical soils

Abstract

This study is devoted to predict water vapour adsorption and hydro-physical properties of arid soils in middle Nile Delta (Farm of the Faculty of Agriculture, Shebin El-Kom, Egypt) and of tropical soils (Felix and INIAP Farms) in Quevedo zone, Los Rios, Ecuador. The vapour pressure and isothermal adsorption of water vapour is used to predict soil moisture adsorption capacity (Wa) and the specific surface area. To achieve these objectives, four soil profiles at different depths were investigated to indicate the status of hydro-physical properties of the studied area.  The 1st & 2nd profiles are sandy loam (Felix Farm) and clay loam soils (Shebin El-Kom Farm), and 3rd & 4th are clay soils (INIAP Farm). Data of soil-water adsorption (W%) at different relative vapor pressures P/Po are obtained for the studied soil profiles, where the W% values increased with increasing P/Po from 1.87% to 10.01% in the 1st and 2nd sandy loam and clay loam soil profiles, and reached 27.44% in the 4th clay soil profile. The highest values of water adsorption capacity (Wa) were observed in the clay depths of 60 – 90 cm and 90 – 120 cm (INIAP-soil profiles) while the lowest values were in the subsurface depth (30 – 60 cm) of soil profiles 1st and 2nd. The other hygro-physical properties such as adsorbed layers and maximum hygroscopic water were obtained. The specific surface area (S) in sandy loam 1st&2nd soil profiles is ranged from 113m2/g to 187m2/g and raised to 385m2/g and 553m2/g in the 3rd & 4th clay soil profiles. The corresponded values of the external specific surface area (Se) ranged from 42m2/g to 98m2/g and 74 m2/g to 252 m2/g respectively. Two equations were assumed (1) to predict P/Po at water adsorption capacity (Wa), and (2) to apply Wa in prediction of soil moisture retention i.e., ѱ(W) function at pF < 4.5.

Keywords

References

  1. Agam, N., Berliner, P.R., 2004. Diurnal water content changes in the bare soil of a coastal desert. Journal of Hydrometeorology 5: 922–933.
  2. Amer, A.M., 1982. Effect of the overburden pressure on the capillary sorption potential of water in swelling soils. PhD Thesis, Faculty of Soil Science, Lomosonov Moscow State University, Moscow, Russia. [in Russian].
  3. Amer, A.M., 1993. Surface area measurements as related to water vapour adsorption in arid soils of Egypt. Proceedings of the IV International Conference on Desert Development. 25-30 July, Mexico City, Mexico. pp. 619–627.
  4. Amer, A.M., 2003. Soil hydro-physics. First Part, Al-Dar Al-Arabia for Publishing Cairo, Egypt. 452p. [in Arabic].
  5. Amer, A.M., 2009. Moisture adsorption capacity and surface area as deduced from vapour pressure isotherms in relation to hygroscopic water of soils. Biologia 64(3): 516-521.
  6. Amer, A.M., 2014. Moisture dynamics and available water capacity in root zone as influenced by swelling pressure and water table in tropical soils. Final Report, submitted to SENESCYT, Prometeo Project, Ecuador.
  7. Amer, A.M., 2015. Vapor adsorption capacity and soil wetting. In: Wetting and wettability. Aliofkhazraei, M. (Ed.). IntechOpen, pp.1-14. Black, G.A., Evans, D.D., White, J.L., Ensminger, L.E., Clerk, F.E., 1965. Methods of soil analysis. Part 1&2. American Society of Agronomy - Soil Science Society of America, Madison, Wisconsin, USA.
  8. Brunauer, S., Emmett, P.H., Teller, E., 1938. Adsorption of gases in multi-molecular layers. Journal of the American Chemical Society 60(2): 309-319.

Details

Primary Language

English

Subjects

-

Journal Section

Research Article

Publication Date

October 1, 2019

Submission Date

December 11, 2018

Acceptance Date

June 18, 2019

Published in Issue

Year 2019 Volume: 8 Number: 4

APA
Amer, A. M. (2019). Soil moisture adsorption capacity and specific surface area in relation to water vapor pressure in arid and tropical soils. Eurasian Journal of Soil Science, 8(4), 289-297. https://doi.org/10.18393/ejss.580889
AMA
1.Amer AM. Soil moisture adsorption capacity and specific surface area in relation to water vapor pressure in arid and tropical soils. EJSS. 2019;8(4):289-297. doi:10.18393/ejss.580889
Chicago
Amer, Abdelmonem Mohamed. 2019. “Soil Moisture Adsorption Capacity and Specific Surface Area in Relation to Water Vapor Pressure in Arid and Tropical Soils”. Eurasian Journal of Soil Science 8 (4): 289-97. https://doi.org/10.18393/ejss.580889.
EndNote
Amer AM (October 1, 2019) Soil moisture adsorption capacity and specific surface area in relation to water vapor pressure in arid and tropical soils. Eurasian Journal of Soil Science 8 4 289–297.
IEEE
[1]A. M. Amer, “Soil moisture adsorption capacity and specific surface area in relation to water vapor pressure in arid and tropical soils”, EJSS, vol. 8, no. 4, pp. 289–297, Oct. 2019, doi: 10.18393/ejss.580889.
ISNAD
Amer, Abdelmonem Mohamed. “Soil Moisture Adsorption Capacity and Specific Surface Area in Relation to Water Vapor Pressure in Arid and Tropical Soils”. Eurasian Journal of Soil Science 8/4 (October 1, 2019): 289-297. https://doi.org/10.18393/ejss.580889.
JAMA
1.Amer AM. Soil moisture adsorption capacity and specific surface area in relation to water vapor pressure in arid and tropical soils. EJSS. 2019;8:289–297.
MLA
Amer, Abdelmonem Mohamed. “Soil Moisture Adsorption Capacity and Specific Surface Area in Relation to Water Vapor Pressure in Arid and Tropical Soils”. Eurasian Journal of Soil Science, vol. 8, no. 4, Oct. 2019, pp. 289-97, doi:10.18393/ejss.580889.
Vancouver
1.Abdelmonem Mohamed Amer. Soil moisture adsorption capacity and specific surface area in relation to water vapor pressure in arid and tropical soils. EJSS. 2019 Oct. 1;8(4):289-97. doi:10.18393/ejss.580889

Cited By