2025-02-23T03:36:48-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: Query fl=%2A&wt=json&json.nl=arrarr&q=id%3A%22irk-123456789-5679%22&qt=morelikethis&rows=5
2025-02-23T03:36:48-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: => GET http://localhost:8983/solr/biblio/select?fl=%2A&wt=json&json.nl=arrarr&q=id%3A%22irk-123456789-5679%22&qt=morelikethis&rows=5
2025-02-23T03:36:48-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: <= 200 OK
2025-02-23T03:36:48-05:00 DEBUG: Deserialized SOLR response
Про причини глибинного концентрування вод артезіанських басейнів у зоні гіпергенезу (фізико-хімічний аналіз)
It is shown that different processes of the diffusive nature can participate in the rise of mineralization of the edge water, but baroosmose through fine-porous sediments (rocks) always plays the main role. The intraformational gradient of the osmotic pressure of water is a driving force of baroosmo...
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| Main Author: | |
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| Format: | Article |
| Language: | Ukrainian |
| Published: |
Видавничий дім "Академперіодика" НАН України
2008
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| Subjects: | |
| Online Access: | http://dspace.nbuv.gov.ua/handle/123456789/5679 |
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