2 edition of Moisture equilibria and moisture changes in soils beneath covered areas found in the catalog.
Moisture equilibria and moisture changes in soils beneath covered areas
G. D. Aitchison
Published
1965
by Butterworths in [Sydney]
.
Written in English
Edition Notes
Includes bibliographies.
| Statement | Convened by Soil Mechanics Section, Commonwealth Scientific and Industrial Research Organization, Australia, in collaboration with National Building Research Institute and National Institute for Road Research Council for Scientific and Industrial Research, South Africa. Editor: G. D. Aitchison. |
| Contributions | Commonwealth Scientific and Industrial Research Organization (Australia). Soil Mechanics Section., South African Council for Scientific and Industrial Research. |
| Classifications | |
|---|---|
| LC Classifications | TA710 .A35 |
| The Physical Object | |
| Pagination | 278 p. |
| Number of Pages | 278 |
| ID Numbers | |
| Open Library | OL5954964M |
| LC Control Number | 65028990 |
| OCLC/WorldCa | 10394977 |
cumulation of moisture in a soil subgrade beneath an imper vious surface with the estimated equilibrium moisture contents based on measurements of the moisture retention characteris tics of the soil and the elevation of the groundwater table. Mois ture accumulation due to the formation of ice was not considered. A theoretical approach File Size: 4MB. The soil water regime in a young radiata pine plantaion on a first and second rotation site in south eas Fizicheskie metody ekspressanaliza sostava veshchestvOtv. red. A. D. Skripko] Moisture equilibria and moisture changes in soils beneath covered areas: a .
Moisture is generated inside of basements from people and their activities. Common sources are humidifiers, unvented clothes dryers, showering and cooking. When basements are finished, these activities increase. Another source that can be thought of as internal is the moisture contained in new concrete after construction. In a typical house. In this study, we assess the effects of soil moisture on soil CO 2 and CH 4 production and their δ 13 C values at three soil moisture levels: field capacity, intermediate, and saturation (51%, 77 Cited by:
Richards, B.G. () Determination of the Unsaturated Permeability and Diffusivity Functions from pressure plant outflow data with non-negligible membrane impedance, in Moisture Equilibria and Moisture Changes in Soils Beneath Covered Areas, G.D. Aitchison (ed), a Symposium Convened by Soil Mechanics Section, Commonwealth Scientific and Author: Allen Li, Ken Been, Irwin Wislesky, Terry Eldridge, David Williams. Aitchison G D Engineering concepts of moisture equilibria and moisture changes in soils S. of the Review Panel, ed., Published in Moisture Equilibria and Moisture Changes in Soils Beneath Covered Areas, A Symp,-in-print, Butterworths, Australia Google Scholar.
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Moisture Equilibria and Moisture Changes in Soils Beneath Covered Areas [Aitchison, G.D. (editor)] on *FREE* shipping on qualifying offers. Moisture Equilibria and Moisture Changes in Soils Beneath Covered AreasAuthor: G.D. (editor) Aitchison. Get this from a library.
Moisture equilibria and moisture changes in soils beneath covered areas; a symposium in print. [G D Aitchison; CSIRO (Australia).
Soil Mechanics Section.; South African Council for Scientific and Industrial Research.]. Moisture equilibria and moisture changes in soils beneath covered areas.
A Symposium In Print Convened By Commonwealth Scientific And Industrial Research Organization. Soil Mechanics Section, In Collaboration With National Building Research Institute And National Institute For Road Research, Council For Scientific And Industrial Research, South by: MOISTURE EQUILIBRIA AND MOISTURE CHANGES IN SOILS BENEATH COVERED AREAS - A SYMPOSIUM IN PRINT - CONVENED BY THE SOIL MECHANICS SECTION, COMMONWEALTH SCIENTIFIC AND INDUSTRIAL RESEARCH ORGANIZATION AUSTRALIA ETC By: AITCHISON, G.
Books ordered may be returned for a full refund if they are not as .Moisture equilibria and moisture changes in soils beneath covered areas: a symposium in print / edited by Gordon D.
Aitchison Butterworths Sydney Wikipedia Citation Please see Wikipedia's template documentation for further citation fields that may be required. Moisture equilibria and moisture changes in soils beneath covered areas: a symposium in print / edited by Gordon D.
Aitchison Aitchison, G. D View online Borrow. Equilibrium moisture beneath highway pavements is critical to pavement design because moisture directly affects the strength and stiffness of pavement systems.
Moisture is related to soil suction. Soil samples were obtained from the two main residual soil formations, the Jurong sedimentary formation and the Bukit Timah granitic formation, at various depths.
The effect of weathering on the shape of the soil—water characteristic curve is by: Monitoring Long-Term Subgrade Moisture Changes with Electrical Resistivity Tomography the edge moisture variation distance, the long-term equilibrium moisture beneath the covered area, and seasonal fluctuations of moisture at the edge.
Changes in the Soil Moisture Characteristic due to Porosity Variation. Engineering concepts of moisture equilibria and moisture changes in soils Engineering concepts of moisture equilibria and moisture changes in soils. Published. 1 June from Australia, Great Britain, Israel and S. Africa convened in to review the state of knowledge on moisture in soils under roads and buildings in areas where.
Moisture Equilibria and Moisture Changes in Soils Beneath Covered Areas. Appears in 8 books from Page - Yoshida, RT, Fredlund, DG, and Hamilton, JJ AITCHISON, G. Review Panel Statement - Engineering Concepts of Moisture Equilibria and Moisture Changes in Soils.
In: Conf. on Moisture Equilibria and Moisture Changes in Soil Beneath Covered Areas, 1. London, England. Proceedings London: Butterworths,p. AITCHISON, G. The quantitative description of the stress. Aitchison, G.D.
(Editor). Moisture equilibria and moisture changes in soils beneath covered areas. A Symposium in Print. Butterworths, Australia. Google ScholarCited by: AITCHISON, G.D. Review panel statement – engineering concepts of moisture equilibria and moisture changes in soils.
In: Conference on Moisture Equilibria and Moisture Changes in Soils Beneath Covered Areas, v.1, p, AITCHINSON, G. The quantitative description of the stress-deformation behavior of expansive soils.
C. Bruijn Particle De () Some observations on soil moisture conditions beneath and adjacent to tarred roads and other surface treatments in South Africa G. Aitchison (Eds) Moisture Equilibria and Moisture Changes in Soils Beneath Covered Areas Butterworth Sydney, Australia –Cited by: //Aitchison G.
Moisture Equilibria and Moisture Changes in Soils Beneath Covered Areas. Sydney: Butterworth, A revised effective stress law.
Vertical moisture barriers have the potential to stabilize the moisture variations beneath covered areas (e.g., pavements, slab-on-ground foundations, etc.) in response to surface moisture flux boundary conditions, and can affectively be used in controlling the volume changes of expansive soils with wetting and drying cycles.
Development of a mechanistic-empirical model to predict equilibrium suction for subgrade soil. Moisture Equilibria and Moisture Changes in Soil Beneath Covered Areas, Butterworths, Sydney (), pp.
Google Scholar. Moisture Equilibria and Moisture Changes in Soils Beneath Covered Areas, Sydney, Butterworths (), pp. Author: Sajib Saha, Narain Hariharan, Fan Gu, Xue Luo, Dallas N.
Little, Robert L. Lytton. [4] K. Russam, The prediction of subgrade moisture conditions for design purposes, Moisture equilibria and moisture changes in soils beneath covered areas.
Proceedings of the conference, Australia by: 1. When the drying time is short as shown in Fig. 3(a), the zone with the suction change is limited to the area beneath the horizontal moisture barrier.
As the drying time increases as shown in Fig. 3(b), the zone with the suction change expands towards the pavement slab. Numerical Analysis of Horizontal Moisture Barriers in Pavements Constructed Cited by: 2.
"Complements the introductory volume to the Conference entitled: 'Moisture equilibria and moisture changes in soils beneath covered areas'." Description: pages: illustrations ; 29 cm: Responsibility.DETERMINING MOISTURE CONTENT IN SOIL MATERIALS TXDOT DESIGNATION: TEXE CONSTRUCTION DIVISION 2 – 7 LAST REVIEWED: SEPTEMBER Class G2 in accordance with TexK for specimens with a mass greater than g.
Specimen containers for conventional ovens, with close fitting lids if specimen is less than g. File Size: 96KB.Since the heat conductivity of a soil increases with its moisture content, the size of the current through the microammeter is an index of the amount of moisture in the soil.
In studying soil moisture changes in the laboratory, soil was placed in a cylindrical woven-wire - 16 - container lined with linen, the soil arm of the bridge was inserted.
