Thermodynamic characteristics of the water weakly bound with the surface of layer silicates (Record no. 160874)
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| 000 -LEADER | |
|---|---|
| fixed length control field | 01662nam a22002417a 4500 |
| 003 - CONTROL NUMBER IDENTIFIER | |
| control field | ZW-GwMSU |
| 005 - DATE AND TIME OF LATEST TRANSACTION | |
| control field | 20230215111818.0 |
| 008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION | |
| fixed length control field | 230215b |||||||| |||| 00| 0 eng d |
| 040 ## - CATALOGING SOURCE | |
| Original cataloging agency | MSU |
| Transcribing agency | MSU |
| Description conventions | rda |
| 100 ## - MAIN ENTRY--PERSONAL NAME | |
| Personal name | TARASEVICH, Yu. I |
| 245 ## - TITLE STATEMENT | |
| Title | Thermodynamic characteristics of the water weakly bound with the surface of layer silicates |
| 264 ## - PRODUCTION, PUBLICATION, DISTRIBUTION, MANUFACTURE, AND COPYRIGHT NOTICE | |
| Place of production, publication, distribution, manufacture | Kiev |
| Name of producer, publisher, distributor, manufacturer | Allerton Press |
| Date of production, publication, distribution, manufacture, or copyright notice | 2013 |
| 336 ## - CONTENT TYPE | |
| Source | rdacontent |
| Content type term | text |
| Content type code | txt |
| 337 ## - MEDIA TYPE | |
| Source | rdamedia |
| Media type term | unmediated |
| Media type code | n |
| 338 ## - CARRIER TYPE | |
| Source | rdacarrier |
| Carrier type term | volume |
| Carrier type code | nc |
| 440 ## - SERIES STATEMENT/ADDED ENTRY--TITLE | |
| Title | Journal of Water Chemistry and Technology |
| Volume/sequential designation | Volume , number , |
| 520 ## - SUMMARY, ETC. | |
| Summary, etc. | The isochoric-isothermal potential ΔF of the interaction of weakly (osmotically) bound water with the kaolinite surface has been determined. In terms of magnitude this potential does not exceed 1.5% of free surface energy of kaolinite. The heat released during the interaction of boundary layers of water with kaolinite is evaluated. This heat is positive (enthalpy −ΔH = Q is negative) and does not exceed 1% of total integral heat of wetting. Entropy ΔS of weakly bound water is determined from the values of ΔF and ΔH.The entropy is compared with the excess entropy of surface layers of liquid water. The positive sign of the entropy indicates a larger disorder of the structure of boundary layers as compared with the bulk phase. Judging from the relationship between ΔH and TΔS the osmotic swelling of clays is determined just by the entropy component of the isochoric-isothermal potential. |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM | |
| Topical term or geographic name entry element | boundary layers |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM | |
| Topical term or geographic name entry element | kaolinite |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM | |
| Topical term or geographic name entry element | montmorillonite |
| 856 ## - ELECTRONIC LOCATION AND ACCESS | |
| Uniform Resource Identifier | https://doi.org/10.3103/S1063455X13030016 |
| 942 ## - ADDED ENTRY ELEMENTS (KOHA) | |
| Source of classification or shelving scheme | Library of Congress Classification |
| Koha item type | Journal Article |
| Withdrawn status | Lost status | Source of classification or shelving scheme | Damaged status | Not for loan | Home library | Current library | Shelving location | Date acquired | Serial Enumeration / chronology | Total Checkouts | Full call number | Date last seen | Price effective from | Koha item type | Public note |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Library of Congress Classification | Main Library | Main Library | - Special Collections | 15/02/2023 | Vol.35 , No.3 (May - Jun 2013) | GB855 JOU | 15/02/2023 | 15/02/2023 | Journal Article | For In House Use Only |