English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Plus monthly

Global: Zendy Tools annual

Global: Zendy Tools monthly

Global: Zendy Free Plan

The data and method of analysis presented here provide for an approximate determination of expected temperature rises. They show that, in general, when large masses of liquid waste are injected into an aquifer through wells, heat conduction is not very significant, and as an approximation the temperature rise within the aquifer, since injection began, is equal to the total heat generated in a unit volume of aquifer divided by the product of the specific gravity of the aquifer and contained waste and its heat capacity. The generalizations outlined here should lead to an understanding of the relative importance of heat storage as compared to thermal conduction away from the region.

Temperature rise within radioactive liquid wastes injected into deep formations