@article{oai:nagoya-wu.repo.nii.ac.jp:00002217,
 author = {八木, 明彦 and 長谷, 成子 and 山田, 久美子 and ヤギ, アキヒコ and ハセ, シゲコ and ヤマダ, クミコ},
 journal = {名古屋女子大学紀要. 家政・自然編, Journal of Nagoya Women's University. Home economics・natural science},
 month = {Mar},
 note = {P(論文), "Lake Fukami-ike is a small lake having a maximum depth of 8.0m, and is well protected from the wind. Lake water stratified from March to October and circulated from November to March. Anoxic condition prevailed below 4-5m depth from April to October. This study was undertaken to clarify in detail the distributions of iron chemical forms in Lake Fukami-ike. The concentration of dissolved iron seemed to be controlled by the balance among the supply of Allochtonous iron, the deposition or dissolution of particulate iron (P-Fe) in the hypolimnion and the FeS fixation at the bottom. The dissolved iron (D-Fe) in the hypolimnion water was specified by ultrafiltration. Percentages of dissolved iron in two molecular weight fractions in depth of 7.0m were 20-30% (M. W. < 5,000), 45-10% (5,000 < M. W. < 100,000) and 5-70% (M. W. > 100,000), respectively. These results indicate that about 50-80% of total dissolved iron was present as the organic form, mainly having a molecular weight of 5,000-100,000, in the hypolimnion of Lake Fukami-ike."},
 pages = {147--154},
 title = {"深見池の成層期における溶存態鉄,懸濁態鉄の存在状態 : 特に溶存有機態鉄について"},
 volume = {41},
 year = {1995}
}