Geoconsolidamenti irreversibili a breve termine
Main Article Content
Abstract
After some consideration, about the geo-dewatering
in use, t h e A. develops new tecniques, following t h e new theoretical bearings
in EGO.
I n fact, when the surface permeability parameter is introduced near
t h e cathode, the A. integrates the classic theories with this assumption,
a t t a i n i n g new deductions, above all applicable, concerning more efficient
consolidations of the layers.
F u n d a m e n t a l deduction is t h a t , in conditions of applicability EGO,
the water conductor effect can be pronounced to the cathode in delay, in respect
to that of EGO.
Such depliasemont takes place, with initial outlining of pure effect
EGO at maximum, more or less acccntuatod, making it possible to self-condition,
rapid and intense consolidated effects of irreversible nature.
Obtaining electroconsolidations at brief terms, at maximum intensity
new s t r u c t u r e s with diagenetic character in function of the dephasement
of the two flux, water migrators (by cathodc) ionic and neutral, in order
of arrival.
in use, t h e A. develops new tecniques, following t h e new theoretical bearings
in EGO.
I n fact, when the surface permeability parameter is introduced near
t h e cathode, the A. integrates the classic theories with this assumption,
a t t a i n i n g new deductions, above all applicable, concerning more efficient
consolidations of the layers.
F u n d a m e n t a l deduction is t h a t , in conditions of applicability EGO,
the water conductor effect can be pronounced to the cathode in delay, in respect
to that of EGO.
Such depliasemont takes place, with initial outlining of pure effect
EGO at maximum, more or less acccntuatod, making it possible to self-condition,
rapid and intense consolidated effects of irreversible nature.
Obtaining electroconsolidations at brief terms, at maximum intensity
new s t r u c t u r e s with diagenetic character in function of the dephasement
of the two flux, water migrators (by cathodc) ionic and neutral, in order
of arrival.
Article Details
How to Cite
BELLUIGI, A. (1975) “Geoconsolidamenti irreversibili a breve termine”, Annals of Geophysics, 28(4), pp. 283–309. doi: 10.4401/ag-4903.
Issue
Section
OLD
Open-Access License
No Permission Required
Istituto Nazionale di Geofisica e Vulcanologia applies the Creative Commons Attribution License (CCAL) to all works we publish.
Under the CCAL, authors retain ownership of the copyright for their article, but authors allow anyone to download, reuse, reprint, modify, distribute, so long as the original authors and source are cited. No permission is required from the authors or the publishers.
In most cases, appropriate attribution can be provided by simply citing the original article.
If the item you plan to reuse is not part of a published article (e.g., a featured issue image), then please indicate the originator of the work, and the volume, issue, and date of the journal in which the item appeared. For any reuse or redistribution of a work, you must also make clear the license terms under which the work was published.
This broad license was developed to facilitate open access to, and free use of, original works of all types. Applying this standard license to your own work will ensure your right to make your work freely and openly available. For queries about the license, please contact ann.geophys@ingv.it.