Laboratory tests of small-diameter HDPE pipes buried in reinforced sand under repeated-load

2008 ◽  
Vol 26 (2) ◽  
pp. 145-163 ◽  
Author(s):  
S.N. Moghaddas Tafreshi ◽  
O. Khalaj
Author(s):  
S.N. Moghaddas Tafreshi ◽  
O. Khalaj ◽  
J. Khanmohammadi

2019 ◽  
Vol 276 ◽  
pp. 05002
Author(s):  
Agus Ika Putra ◽  
Mohamed A. Shahin

The study presented in this paper evaluates the suitability of using slag (with cement) as a stabilizer, for improving the performance of expansive subgrade soil in road pavement. Several laboratory tests were conducted to determine the geotechnical engineering characteristics of the expansive soil and associated mechanical engineering performance. The tests conducted include the particle size distribution, standard Proctor compaction, Atterberg’s limits, free swelling, permeability, California bearing ratio (CBR), unconfined compressive strength (UCS), and repeated load triaxial (RLT). In this study, the use of slag (with cement) as a stabilizer followed three proportion schemes, and the selection of a specific stabilizer proportion was determined based on UCS value that satisfies the required standard as a subgrade for road pavement. The results recommended a stabilizer proportion for the soil studied to be 13.5% slag + 1.5% cement at 28 days curing time. This mixture resulted in a remarkable increase in the UCS value of eight times higher than the UCS value of the non-stabilized soil. The CBR value of the mixture was four times higher than the minimum required value for design of road pavement. The study presented herein confirmed that the exploitation of the by-product material of slag can indeed be useful, both in terms of improving the performance of the subgrade soil for road pavement and sparing the environment a spread of significant potential pollutant.


1996 ◽  
Vol 33 (9) ◽  
pp. 25-30 ◽  
Author(s):  
D. M. Brown ◽  
D. Butler ◽  
N. R. Orman ◽  
J. W. Davies

Currently, little is known about the properties of sanitary gross solids or their transport mechanisms in sewers. This paper describes a project designed to study solids movement in small gravity sewers by laboratory, field and modelling work. Results of laboratory tests on gross solids' transport under steady flow conditions are presented. An ‘idealised’ field-based sewer has been constructed and will be used to monitor solids' movement under non-steady, intermittent flow. A computational model based on a method of characteristics solution of the St Venant equations has been produced. This will be extended to account for solids' erosion, transport and deposition.


Author(s):  
A. B. Hawkins ◽  
I.M. Lloyd ◽  
D. F. T. Nash

AbstractDuring detailed examination of fresh material from split Delft samples extensive mottling was noted in the alluvial deposits at the SERC test bed site at Bothkennar on the Forth Estuary, Scotland. The mottles, invariably related to small diameter holes, are only recognisable for about thirty minutes before becoming indistinguishable due to general oxidation.The mottles have been categorised into fine, medium and coarse size and are recorded by their percentage cover. They show some evidence of cyclic development. Laboratory tests on the mottled material indicate that only the moisture content is significantly affected. Observation of the mottles is important in that they are related to fine holes which in turn will influence the in situ permeability of the material.


Geophysics ◽  
1968 ◽  
Vol 33 (6) ◽  
pp. 1004-1012 ◽  
Author(s):  
Edward A. Sammel

Critical thermal gradients for the onset of convection in small‐diameter wells are computed by means of an expression given by Krige (1939) and are shown graphically for water of several salinities and for glycerol. A series of field and laboratory tests in wells with diameters of 4.8 cm and 10.2 cm showed that water columns are unstable at temperature gradients as low as 0.003 °C/m. Magnitudes of thermal oscillations at higher gradients were as large as 0.49 °C, and apparent sizes of convection cells ranged up to 210 cm in height in a 10.2 cm cylinder and to 48 cm in wells 4.8 cm in diameter. Comparison of temperatures in adjacent wells showed temperature differences as great as 3 °C when thermal gradients were greater than the theoretical critical gradients. It is concluded that temperatures in the upper zone of deep wells may depart widely from ambient temperatures in the formations penetrated.


2019 ◽  
Vol 0 (0) ◽  
pp. 0-0 ◽  
Author(s):  
Pezhman Fazeli Dehkordi ◽  
M. Ghazavi ◽  
Navid Ganjian ◽  
Usama karim

2018 ◽  
Vol 2018 ◽  
pp. 1-11 ◽  
Author(s):  
Jin Liu ◽  
Zezhuo Song ◽  
Yuxia Bai ◽  
Zhihao Chen ◽  
Jihong Wei ◽  
...  

The poor water stability, high penetrability, and low antierosion of sand affect the stability of the sandy soil slope. To understand the effectiveness of environment-friendly organic polymer on these physical properties of sand, a series of laboratory tests including water stability test, penetration test, and runoff erosion test of polymer reinforced sand were performed. The results of tests indicated that the organic polymers have obvious effects on the reinforced sand. The water stability of polymer reinforced sand had been improved strongly. All the reinforced sands with polymer ≥0.3% remained a stable structure at immersing time of 24 hours. The penetrability of the reinforced sand decreased with the increase of the polymer. The reinforced sand with polymer ≥7% was impermeable. The erosion resistance of sand increased with the increase of polymer content. With the polymer ≥4%, the sand surface kept intact with the scouring time more than 2 hours. The results could be applied as the reference for organic polymer reinforced sand engineering, especially for surface protection of embankment, slope, and landfill.


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