The viscosity of basaltic magma; an analysis of field measurements in Makaopuhi lava lake, Hawaii
Clicks: 1
ID: 292567
1968
Article Quality & Performance Metrics
Overall Quality
Not rated
Combines reader engagement with the AI quality analysis. This
article has not been analysed, so there is no overall score —
reader engagement is measured and shown alongside.
Reader Engagement
0.0
/100
1 views
0 readers
AI Quality Assessment
Not analyzed
Readership in this journal
Ranked #3,326 of 8,486 articles by views in american journal of science
Most read
Least read
Bar heights use a square-root scale. Only the 120 most-read articles are drawn; the journal has 8,486 in total.
Mint this article as an NFT
Not yet mintedCreate a permanent, verifiable on-chain record of this article on the Scimatic Network. The NFT is held in your Journament account, and you can withdraw it to your own wallet at any time.
5
SUSD
one-off · no wallet required
Abstract
The methods of rotation viscometry have been applied in the field to a tholeiitic lava at 1130 degrees to 1135 degrees C containing about 25 percent crystals and 2 to 5 percent gas bubbles, using a stainless steel spindle inserted through the lava crust. The results agree well with the Bingham model. Yield values in the lava are 1200 and 700 dynes cm (super -2) , and the plastic constants are 6500 and 7500 poises. Laboratory studies in silicone fluid show gas bubbles enhance plastic behavior. In general, lavas must be treated as non-Newtonian fluids; the conditions that may cause different types of fluid behavior in tholeiitic lava are outlined.
| Reference Key |
openalex_W1966749080
Use this key to autocite in the manuscript while using
SciMatic Manuscript Manager or Thesis Manager
|
|---|---|
| Authors | Herbert R. Shaw, Tim Wright, Dallas L. Peck, R.T. Okamura |
| Journal | american journal of science |
| Year | 1968 |
| DOI |
10.2475/ajs.266.4.225
|
| URL | |
| Keywords | Keywords not found |
Citations
No citations found. To add a citation, contact the admin at info@scimatic.org
Comments
No comments yet. Be the first to comment on this article.