Zobrazeno 1 - 10
of 55
pro vyhledávání: '"Rolf S. Arvidson"'
Publikováno v:
RILEM Technical Letters, Vol 2, Pp 90-98 (2017)
Recent advances in bridging kinetics and thermodynamics of mineral dissolution have opened new horizons in our understanding of the role of dissolution in cement hydration. Indeed most hydration kinetic regimes of alite can be rationally envisioned f
Externí odkaz:
https://doaj.org/article/cb0d575eb0a34d668b5843412d2e67a4
Publikováno v:
Geochimica et Cosmochimica Acta. 309:329-351
Intrinsic heterogeneities of crystals almost always impose challenges on the investigation of dissolution kinetics. In the case of the incomplete solid solution series of alkali feldspars, additional complexity to the wide range in chemical compositi
Autor:
Cornelius Fischer, Rolf S. Arvidson
Publikováno v:
American Journal of Science. 320:iii-vi
Publikováno v:
Chemical Geology. 504:216-235
In a unique “perspectives” format that examines both past and future, we appraise the field of crystal dissolution kinetics, showing how the last century's strong progress in experimental discovery has both driven, and been driven by, the tandem
Publikováno v:
PLoS Biology, Vol 3, Iss 3, p e77 (2005)
The deep-sea vestimentiferan tubeworm Lamellibrachia luymesi forms large aggregations at hydrocarbon seeps in the Gulf of Mexico that may persist for over 250 y. Here, we present the results of a diagenetic model in which tubeworm aggregation persist
Externí odkaz:
https://doaj.org/article/6b47af89baaa4e11a475c5dd2b0c5ed1
Publikováno v:
RILEM Technical Letters, Vol 2, Pp 90-98 (2017)
Recent advances in bridging kinetics and thermodynamics of mineral dissolution have opened new horizons in our understanding of the role of dissolution in cement hydration. Indeed most hydration kinetic regimes of alite can be rationally envisioned f
Publikováno v:
Geochimica et Cosmochimica Acta. 212:167-175
Crystal size is an important parameter for many geochemical processes, and is often observed to have a significant influence on crystal dissolution rate. Although size versus solubility relationships are often cast in thermodynamic terms (the critica
Publikováno v:
Minerals
Volume 8
Issue 6
Minerals, Vol 8, Iss 6, p 256 (2018)
Minerals 8(2018)6, 256
Volume 8
Issue 6
Minerals, Vol 8, Iss 6, p 256 (2018)
Minerals 8(2018)6, 256
This brief paper presents a rare dataset: a set of quantitative, topographic measurements of a dissolving calcite crystal over a relatively large and fixed field of view (~400 &mu
m2) and long total reaction time (>
6 
h). Using
m2) and long total reaction time (>
6 
h). Using
Publikováno v:
Aquatic Geochemistry. 21:415-422
We compare the canonical treatment of calcite’s dissolution rate from the literature in a closed system, particle batch reactor, with the alternative approach suggested by Truesdale (Aquat Geochem, 2015). We show that the decay of rate over time ca
Publikováno v:
Aquatic Geochemistry. 20:343-362
The onset of pelagic sedimentation attending the radiation of pelagic calcifiers during the Mesozoic was an important divide in Earth history, shifting the locus of significant carbonate sedimentation from the shallow shelf environments of the Paleoz