FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4304127921> ?p ?o ?g. }

• W4304127921 endingPage "7440" @default.
• W4304127921 startingPage "7440" @default.
• W4304127921 abstract "The sorption behavior and spatial microdistribution of Cs-137, Sr-90 and Am-241 onto the surface of a fractured rock sample from the R-11 borehole of the exocontact zone of the Nizhnekansky granitoid massif were studied. The sorption efficiency of the fractured sample increases in the row of Sr < Cs < Am, where americium is the most retained radionuclide. Based on the image processing of radiograms and scanning electron microscopy data, the mineral relative sorption efficiency (RSE) values were determined to quantify the contribution of the mineral phases of the fractured sample to radionuclide retention. It was established that cesium and strontium are predominantly retained in cracks filled with secondary mineral chlorite. Zeolite is a less effective sorbent with respect to cesium and strontium. Americium sorption is uniform over the whole surface of the fractured sample, with close RSE values for all mineral phases (RSE ~1). The behavior of cesium in heterogeneous and monomineral systems of crushed mineral phases of quartz, biotite and zeolite NaA imitating minerals of the fractured rock sample R-11 was determined. It was shown that the fraction of the sorbed cesium in a heterogeneous system of two mineral phases—biotite and quartz—was larger than the sum of sorption values for the same separated mineral phases. Based on the models of radionuclide sorption on illite–smectite minerals, it was able to estimate the depth of the penetration of solution into the fractured rock sample R-11. The variations of penetration depths for solutions of specific radionuclide into the fractured rock sample were established." @default.
• W4304127921 created "2022-10-11" @default.
• W4304127921 creator A5002494657 @default.
• W4304127921 creator A5017455610 @default.
• W4304127921 creator A5037987302 @default.
• W4304127921 creator A5059781597 @default.
• W4304127921 creator A5065375710 @default.
• W4304127921 creator A5067479296 @default.
• W4304127921 creator A5089878122 @default.
• W4304127921 creator A5090205862 @default.
• W4304127921 date "2022-10-10" @default.
• W4304127921 modified "2023-09-26" @default.
• W4304127921 title "Sorption and Spatial Distribution of 137Cs, 90Sr and 241Am on Mineral Phases of Fractured Rocks of Nizhnekansky Granitoid Massif" @default.
• W4304127921 cites W1674042760 @default.
• W4304127921 cites W1914187162 @default.
• W4304127921 cites W1916330874 @default.
• W4304127921 cites W1966250954 @default.
• W4304127921 cites W1972637513 @default.
• W4304127921 cites W1976579496 @default.
• W4304127921 cites W1981317791 @default.
• W4304127921 cites W1986545444 @default.
• W4304127921 cites W1988329431 @default.
• W4304127921 cites W1993742331 @default.
• W4304127921 cites W2001620199 @default.
• W4304127921 cites W2024481203 @default.
• W4304127921 cites W2033251150 @default.
• W4304127921 cites W2048028584 @default.
• W4304127921 cites W2050239113 @default.
• W4304127921 cites W2074068129 @default.
• W4304127921 cites W2084493034 @default.
• W4304127921 cites W2086212056 @default.
• W4304127921 cites W2131838410 @default.
• W4304127921 cites W2315830841 @default.
• W4304127921 cites W2328852561 @default.
• W4304127921 cites W2477101216 @default.
• W4304127921 cites W2558393424 @default.
• W4304127921 cites W2793423456 @default.
• W4304127921 cites W2887149208 @default.
• W4304127921 cites W2898643157 @default.
• W4304127921 cites W2900600906 @default.
• W4304127921 cites W2938533537 @default.
• W4304127921 cites W2965440499 @default.
• W4304127921 cites W2968960100 @default.
• W4304127921 cites W2995784187 @default.
• W4304127921 cites W3003645495 @default.
• W4304127921 cites W3095785576 @default.
• W4304127921 cites W4241533599 @default.
• W4304127921 cites W97358485 @default.
• W4304127921 doi "https://doi.org/10.3390/en15197440" @default.
• W4304127921 hasPublicationYear "2022" @default.
• W4304127921 type Work @default.
• W4304127921 citedByCount "0" @default.
• W4304127921 crossrefType "journal-article" @default.
• W4304127921 hasAuthorship W4304127921A5002494657 @default.
• W4304127921 hasAuthorship W4304127921A5017455610 @default.
• W4304127921 hasAuthorship W4304127921A5037987302 @default.
• W4304127921 hasAuthorship W4304127921A5059781597 @default.
• W4304127921 hasAuthorship W4304127921A5065375710 @default.
• W4304127921 hasAuthorship W4304127921A5067479296 @default.
• W4304127921 hasAuthorship W4304127921A5089878122 @default.
• W4304127921 hasAuthorship W4304127921A5090205862 @default.
• W4304127921 hasBestOaLocation W43041279211 @default.
• W4304127921 hasConcept C121332964 @default.
• W4304127921 hasConcept C127313418 @default.
• W4304127921 hasConcept C150394285 @default.
• W4304127921 hasConcept C151730666 @default.
• W4304127921 hasConcept C158973077 @default.
• W4304127921 hasConcept C160776313 @default.
• W4304127921 hasConcept C161790260 @default.
• W4304127921 hasConcept C17409809 @default.
• W4304127921 hasConcept C177322064 @default.
• W4304127921 hasConcept C178790620 @default.
• W4304127921 hasConcept C179104552 @default.
• W4304127921 hasConcept C185592680 @default.
• W4304127921 hasConcept C192552737 @default.
• W4304127921 hasConcept C199289684 @default.
• W4304127921 hasConcept C2775859737 @default.
• W4304127921 hasConcept C2776432453 @default.
• W4304127921 hasConcept C2776581184 @default.
• W4304127921 hasConcept C2777229588 @default.
• W4304127921 hasConcept C2777844515 @default.
• W4304127921 hasConcept C2778077586 @default.
• W4304127921 hasConcept C2779429093 @default.
• W4304127921 hasConcept C2779870107 @default.
• W4304127921 hasConcept C2779899878 @default.
• W4304127921 hasConcept C40212044 @default.
• W4304127921 hasConcept C43617362 @default.
• W4304127921 hasConcept C518915863 @default.
• W4304127921 hasConcept C519659679 @default.
• W4304127921 hasConcept C540271850 @default.
• W4304127921 hasConcept C552554468 @default.
• W4304127921 hasConcept C55493867 @default.
• W4304127921 hasConcept C58445606 @default.
• W4304127921 hasConcept C62520636 @default.
• W4304127921 hasConceptScore W4304127921C121332964 @default.
• W4304127921 hasConceptScore W4304127921C127313418 @default.
• W4304127921 hasConceptScore W4304127921C150394285 @default.
• W4304127921 hasConceptScore W4304127921C151730666 @default.

• next