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1 d porous mineral surfaces and their roles in chemical evolution.
2 ing the Moon's formation and its thermal and chemical evolution.
3 and may be restricted to galaxies of limited chemical evolution.
4 this is, we state, the last possible step of chemical evolution.
5 nization of the material and consequently to chemical evolution.
6 e previous work that aimed to understand the chemical evolution (aging) of POA and SOA has focused on
9 timescales is crucial for understanding the chemical evolution and thermal histories of terrestrial
10 and other optical properties to examine the chemical evolution and transformation of oil components
11 rstellar medium (after allowing for Galactic chemical evolution), and indicates that the absorption s
12 f some of the chemical processes involved in chemical evolution, and a partial answer to the fundamen
14 the establishment of prebiotic attributes in chemical evolution as well as the origin of terrestrial
21 etween planets with parallel chemistries and chemical evolution could in principle amplify the develo
22 time that would have been required for early chemical evolution, countering the view that not enough
23 ation environments in comet-forming regions, chemical evolution during their long storage in reservoi
24 erials is largely governed by structural and chemical evolutions during electrochemical reactions.
25 a surface reduced layer, to transition) and chemical evolution (formation of a surface reaction laye
26 abiogenesis (the development of life through chemical evolution from inorganic materials) can be esti
30 for the study of surface reconstruction and chemical evolution in battery materials using combined d
31 of these monomers, the ice world (i.e., the chemical evolution in the range between the freezing poi
35 osited on the surface of the oceans, further chemical evolution might have transformed these molecule
37 deuterium is destroyed in stellar interiors, chemical evolution models predict that its Galactic Cent
38 used a one-dimensional model to simulate the chemical evolution of air masses in the tropical Atlanti
39 resolved mass that describe the physical and chemical evolution of aircraft exhaust plumes on the tim
41 of such water on the physical properties and chemical evolution of Earth's interior, it is essential
44 t affect arsenic concentrations, such as the chemical evolution of groundwater, redox differences, an
48 od that possesses the ability to monitor the chemical evolution of supercritical CO(2) in relevant co
49 ord important information on the thermal and chemical evolution of the Archean-Proterozoic Earth.
50 (HCCCCH) and triacetylene (HCCCCCCH) in the chemical evolution of the atmosphere of Saturn's moon Ti
53 ization approach to study the structural and chemical evolution of the metal sulfide-utilizing powder
56 resulting elucidation of the structural and chemical evolution of the system leads to a new descript
57 re we track three-dimensional structural and chemical evolution of tin anodes in sodium-ion batteries
58 he role of these key reaction classes in the chemical evolution of Titan's orange-brownish haze layer
62 sotopic reservoir but they diverged in their chemical evolution owing to subsequent fractionation by
63 s, provides insight to the morphological and chemical evolution pathways leading to core-shell partic
64 een hypothesized as an ordering principle in chemical evolution, rather than chemical evolution by na
65 ovide insight into an outcome of early solar chemical evolution that differs from any seen so far in
69 e to analyze structural characterization and chemical evolution with its powerful and unique applicat
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