bighouse
Civil/Environmental
- Oct 10, 2013
- 4
I have been performing in-situ permeability tests in the field and have sporadically been getting permeability coefficients that have been inconsistent with the soil type.
The onsite soils are generally dense to very dense glacial end moraine and outwash deposits of gravel and sand with frequent cobbles, occasional boulders, and trace amounts of silt. Some of the specific USCS classifications based on laboratory testing and the corresponding coefficient of permeability values (Kv) are listed below. The samples submitted for laboratory testing were obtained using a 3” spoon at the test depth (ie run a permeability test at 10 ft and then sample from 10 ft to 12 ft).
GP – Kv = 5.9x10-5 cm/s
SP – Kv = 9.0x10-5 cm/s
SP-SM – Kv = 7.7x10-3 cm/s
SP – Kv = 4.2x10-4 cm/s
GW – Kv = 1.2x10-3 cm/s
GP-GM – Kv = 8.2x10-5 cm/s
The permeability tests are falling head tests run through a 4” casing flush with the bottom of the hole (ie we pound the casing to 10 ft, clear then hole out to 10 ft and then run a permeability test at 10 ft). The test procedure roughly follows ASTM D6391, method B.
In the tops of some of the samples we have been noting coarse gravel and cobble pieces which I suspect may be reducing the effective opening size (ie a 2.5” piece of gravel may be obstructing the casing opening). However, I find it hard to believe that such an obstruction would have such a dramatic impact on the permeability rate (reducing it by a power of 100 or 1000) unless the casing was sitting flush on top of a cobble or boulder which we haven’t been seeing.
Is it possible that this material could actually have such a low permeability? Or has anyone had similar trouble with this test or in-situ permeability tests in general? If so, what was the problem and how did you resolve it?
Any suggestions are greatly appreciated.
The onsite soils are generally dense to very dense glacial end moraine and outwash deposits of gravel and sand with frequent cobbles, occasional boulders, and trace amounts of silt. Some of the specific USCS classifications based on laboratory testing and the corresponding coefficient of permeability values (Kv) are listed below. The samples submitted for laboratory testing were obtained using a 3” spoon at the test depth (ie run a permeability test at 10 ft and then sample from 10 ft to 12 ft).
GP – Kv = 5.9x10-5 cm/s
SP – Kv = 9.0x10-5 cm/s
SP-SM – Kv = 7.7x10-3 cm/s
SP – Kv = 4.2x10-4 cm/s
GW – Kv = 1.2x10-3 cm/s
GP-GM – Kv = 8.2x10-5 cm/s
The permeability tests are falling head tests run through a 4” casing flush with the bottom of the hole (ie we pound the casing to 10 ft, clear then hole out to 10 ft and then run a permeability test at 10 ft). The test procedure roughly follows ASTM D6391, method B.
In the tops of some of the samples we have been noting coarse gravel and cobble pieces which I suspect may be reducing the effective opening size (ie a 2.5” piece of gravel may be obstructing the casing opening). However, I find it hard to believe that such an obstruction would have such a dramatic impact on the permeability rate (reducing it by a power of 100 or 1000) unless the casing was sitting flush on top of a cobble or boulder which we haven’t been seeing.
Is it possible that this material could actually have such a low permeability? Or has anyone had similar trouble with this test or in-situ permeability tests in general? If so, what was the problem and how did you resolve it?
Any suggestions are greatly appreciated.