A
Anja Røyne
Researcher at University of Oslo
Publications - 50
Citations - 2180
Anja Røyne is an academic researcher from University of Oslo. The author has contributed to research in topics: Calcite & Carbonate. The author has an hindex of 18, co-authored 48 publications receiving 1797 citations. Previous affiliations of Anja Røyne include University of Sydney.
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Cooling of photovoltaic cells under concentrated illumination: a critical review
TL;DR: In this paper, the authors present an overview of various cooling methods that can be employed for photovoltaic cells, including linear concentrators, single-cell arrangements, and densely packed photovolastic cells.
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Developing a general interaction potential for hydrophobic and hydrophilic interactions
Stephen H. Donaldson,Anja Røyne,Kai Kristiansen,Michael V. Rapp,Saurabh Das,Matthew A. Gebbie,Dong Woog Lee,Philipp Stock,Markus Valtiner,Jacob N. Israelachvili +9 more
TL;DR: In this article, direct force measurements on a broad class of hydrophobic and hydrophilic surfaces have enabled the development of a general interaction potential per unit area, W(D) = −2γiHy exp(−D/DH).
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Design of a jet impingement cooling device for densely packed PV cells under high concentration
Anja Røyne,Christopher Dey +1 more
TL;DR: In this paper, a cooling device based on jet impingement is proposed for cooling of densely packed photovoltaic cells under high concentration, which consists of an array of jets where the cooling fluid is drained around the sides in the direction normal to the surface.
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The interface-scale mechanism of reaction-induced fracturing during serpentinization
TL;DR: In this article, a microstructurally consistent, self-propagating fracture mechanism was proposed, driven by the growth and transformation of a metastable amorphous proto-serpentine phase, where stress is localized within surface perturbations (etch pits and coalesced etch pits).
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Controls on rock weathering rates by reaction-induced hierarchical fracturing
TL;DR: In this article, the observed spheroidal weathering patterns in basaltic intrusions (dolerites) in the Karoo Basin in South Africa are created through volume expanding reactions which set up stresses that not only lead to spalling of spheroroidal layers of rock, but also drive a large scale hierarchical fracturing process by which the dolerite is continuously undergoing domain division.