Zobrazeno 1 - 10
of 43
pro vyhledávání: '"Motoharu Kawano"'
Autor:
Motoharu KAWANO, Jinyeon HWANG
Publikováno v:
Journal of Mineralogical and Petrological Sciences. 118
Autor:
MOTOHARU KAWANO, YASUYUKI KOYAMA
Publikováno v:
Clay Science; 2023, Vol. 27 Issue 1/2, p17-24, 8p
Autor:
Eri Yamada, Motoharu Kawano
Publikováno v:
Clays and Clay Minerals. 66:370-378
Citrate is distributed widely in the Earth’s surface environments as a biological product released by microbes and plants. Citrate is also often used as a chelating agent for the selective dissolution of iron coatings and free iron oxides in soils.
Publikováno v:
Journal of Mineralogical and Petrological Sciences. 113:207-217
Autor:
Tomoaki Maeda, Motoharu Kawano
Publikováno v:
Journal of Crystal Growth. 535:125536
Selenic acid (Se(IV)), arsenic acid (As(V)), and silicic acid are widespread oxyanions in some Earth’s surface environments. To evaluate the effect of these oxyanions on the polymorphism and precipitation rate of calcium carbonate (CaCO3) minerals,
Autor:
Motoharu Kawano, Jinyeon Hwang
Publikováno v:
Clays and Clay Minerals. 69:797-797
This article was updated to fix formatting errors in Eqs. 1, 2 and 3 introduced in the production process.
Autor:
Motoharu Kawano, Eri Yamada
Publikováno v:
Clays and Clay Minerals.
Autor:
Motoharu Kawano, Jinyeon Hwang
Publikováno v:
Applied Clay Science. 51:484-490
Organic molecules secreted by bacterial cells are capable of influencing dissolution and precipitation rates of various minerals including calcium carbonate (CaCO 3 ) minerals. To evaluate the effects of polysaccharides on the precipitation rates and
Autor:
Katsutoshi Tomita, Motoharu Kawano
Publikováno v:
Clays and Clay Minerals. 50:99-110
Bacterial mineralization in weathered pyroclastic deposits of the Kaimondake volcanic ash (4040 ybp) and the Koya pyroclastic flow (6400 ybp) was investigated to evaluate the impacts of bacteria on mineral formation, and to characterize the microbiog
Autor:
Katsutoshi Tomita, Motoharu Kawano
Publikováno v:
American Mineralogist. 86:1156-1165
Mineralogy and geochemistry of a sulfuric acid spring water with a pH of 3.37 to 2.89 were investigated to verify the formation processes of iron minerals and the effects of bacteria on their formation. To estimate the solubility of schwertmannite, e