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Hydro-Mechanical Properties of an Unsaturated Frictional Material

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128 CHAPTER 6. EXPERIMENTAL RESULTS<br />

suddenly applied to <strong>an</strong> initially saturated specimen) it seems, that the parameters as air-entry<br />

value, residual suction, residual water content <strong>an</strong>d water-entry value are similar for the loose<br />

specimens <strong>an</strong>d respectively for the dense specimens.<br />

6.3 <strong>Unsaturated</strong> Hydraulic Conductivity<br />

The unsaturated hydraulic conductivity was directly determined using suction <strong>an</strong>d also volu-<br />

metric water content measurements from the tr<strong>an</strong>sient state s<strong>an</strong>d column test I. Exemplary<br />

pore-water pressure (hydrostatic pressure has positive sign <strong>an</strong>d matric suction has negative<br />

sign) <strong>an</strong>d also exemplary volumetric water content pr<strong>of</strong>iles are presented in Fig. 6.13 for initial<br />

drainage process <strong>an</strong>d in Fig. 6.14 for 1 st drainage process <strong>of</strong> loose specimen. Measurements<br />

every 20 th minutes are presented for several depths. Fig. 6.13 presents the initial condition<br />

which is a fully saturated specimen. The tensiometer sensors measure the hydrostatic pres-<br />

sure (positive pore water pressure) <strong>of</strong> water that shows a linear distribution in the specimen.<br />

The TDR sensors measure the volumetric water content that is const<strong>an</strong>t along the column.<br />

Fig. 6.14 also presents a saturated specimen with a linear distributed positive pore water<br />

pressure. But after 1 st imbibition process air remains in the pores <strong>an</strong>d therefore full satu-<br />

ration <strong>of</strong> the specimen is not reached (θ ′ s = 39%) as given in the volumetric water content<br />

pr<strong>of</strong>ile. Only the bottom TDR sensor is located in the saturated zone through the experiment<br />

(θs = 46%). Both Figures show with outflow <strong>of</strong> water decreasing pore water pressure <strong>an</strong>d<br />

decreasing volumetric water content first in the top part <strong>an</strong>d then in the bottom part <strong>of</strong> the<br />

specimen.<br />

Depth (cm)<br />

0<br />

10<br />

20<br />

30<br />

40<br />

50<br />

6<br />

4<br />

state 30 min 120 min 180 min Initial<br />

min 300 min 360 min 420 min 240<br />

Pore - water pressure (kPa)<br />

2<br />

0<br />

-2<br />

-4<br />

-6<br />

0<br />

10<br />

20<br />

30<br />

40<br />

50<br />

50<br />

Volumetric water content (%)<br />

40<br />

30<br />

20<br />

10<br />

Initial drainage<br />

Loose specimen<br />

Initial void ratio = 0.89<br />

Figure 6.13: Pore-water pressure <strong>an</strong>d volumetric water content pr<strong>of</strong>iles for initial drainage<br />

process (loose specimen)<br />

0

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