Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Shigeto Nakabayashi"'
Autor:
Mamiko Mochizuki, Sei-Ichi Saitoh, Kohsei Sasaoka, Masashi Kusakabe, Kenshi Kuma, Naonobu Shiga, Shigeto Nakabayashi
Publikováno v:
Limnology and Oceanography. 47:885-892
Vertical distributions of Fe(III) hydroxide solubilities (
Publikováno v:
Geophysical Research Letters. 28:4611-4614
Detailed vertical distributions of Fe(III) hydroxide solubilities and dissolved Fe concentrations, which are strongly related to the concentration and affinity of natural organic Fe(III) chelators in seawater, were measured at three typical stations
Publikováno v:
Marine Chemistry. 68:231-247
Radiocarbon of carbonate (PIC) and of organic carbon (POC) in sediment trap samples from the Okinawa trough was measured by AMS. Concentrations of 14 C in PIC and POC ( Δ 14 C -PIC and Δ 14 C -POC) ranged from approximately +40‰ to −80‰ and a
Publikováno v:
Water Research. 29:1559-1569
The photoreduction of Fe(III) in seawater (pH 8.1) has been investigated over a range of natural sunlight intensities at 5, 10 and 15°C in the presence of hydroxycarboxylic acid (HCA), such as sugar acids. The Fe(III) photoreduction abilities of HCA
Publikováno v:
Analytica Chimica Acta. 271:25-29
A liquid chromatographic (LC) method with flurescence detection was developed with sufficient sensitivity to determine organic acids in sea water and sediments. Sugar acids, except for uronic and α-keto acids, have not previously been measured in se
Publikováno v:
Marine Chemistry. 40:273-289
The distribution of manganese was investigated during a spring bloom in Funka Bay by chemically segregating dissolved, soluble and refractory Mn. The concentration of dissolved Mn changed slightly owing to assimilation by phytoplankton and dissolutio
Publikováno v:
Marine Chemistry. 38:133-143
Dissolution rate constants and solubilities of colloidal hydrous ferric oxide in seawater over the pH range 5.5–8.1 at 20°C were experimentally determined by dialysis techniques involving γ-activity measurements of 59Fe. The Fe(III) dissolution r
Publikováno v:
Marine Chemistry. 37:15-27
Fe(III) in seawater was readily reduced to Fe(II) in sunlight in the presence of hydroxycarboxylic acids, such as sugar acids. Tartaric, gluconic, glucaric acids and glucaric acid-1,4-lactone gave higher reduced Fe(II) concentrations and a more rapid
Autor:
Kenshi Kuma, Takeshi Yoshimura, Jun Nishioka, Takeshi Nakatsuka, Humio Mitsudera, Daisuke Tsumune, Koji Suzuki, W. Keith Johnson, Tsuneo Ono, Shigeto Nakabayashi, Hiroaki Saito, Shigenobu Takeda, Atsushi Tsuda
Publikováno v:
Journal of Geophysical Research. 112
[1] Iron is an essential nutrient and plays an important role in the control of phytoplankton growth (Martin et al., 1989). Atmospheric dust has been thought to be the most important source of iron, supporting annual biological production in the west
Publikováno v:
Journal of Geophysical Research. 108
[1] The vertical profiles of nutrient, AOU (apparent oxygen utilization), and Fe(III) hydroxide solubility (Fe(III) solubility) in the western North Pacific commonly show that their concentrations increased with depth below the surface mixed layer an