Factors explaining the yearly changes in minimum bottom dissolved oxygen concentrations in Lake Biwa, a warm monomictic lake.


Journal

Scientific reports
ISSN: 2045-2322
Titre abrégé: Sci Rep
Pays: England
ID NLM: 101563288

Informations de publication

Date de publication:
22 01 2019
Historique:
received: 04 04 2018
accepted: 23 11 2018
entrez: 24 1 2019
pubmed: 24 1 2019
medline: 24 1 2019
Statut: epublish

Résumé

Vertical profiles of dissolved oxygen (DO) and water temperature (WT) measured bi-monthly for 36 years (1980-2015) near the deepest part of a warm monomictic lake were analyzed with special reference to yearly minimum DO at bottom (DOmin). DOmin changed yearly (3.0 ± 1.2 mg l

Identifiants

pubmed: 30670746
doi: 10.1038/s41598-018-36533-7
pii: 10.1038/s41598-018-36533-7
pmc: PMC6342936
doi:

Types de publication

Journal Article Research Support, Non-U.S. Gov't

Langues

eng

Sous-ensembles de citation

IM

Pagination

298

Références

Anal Sci. 2012;28(7):675-81
pubmed: 22790369
Environ Sci Technol. 2012 Sep 18;46(18):9964-71
pubmed: 22871037

Auteurs

Takehiko Fukushima (T)

Faculty of Life and Environmental Sciences, University of Tsukuba, 1-1-1 Tennodai, Tsukuba, 305-8572, Japan. fukushima.takehik.fu@u.tsukuba.ac.jp.
Ibaraki Kasumigaura Environmental Science Center, 1853 Okijyuku-machi, Tsuchiura, 300-0023, Japan. fukushima.takehik.fu@u.tsukuba.ac.jp.

Tomohiro Inomata (T)

Faculty of Life and Environmental Sciences, University of Tsukuba, 1-1-1 Tennodai, Tsukuba, 305-8572, Japan.

Eiji Komatsu (E)

LERCS Co., 5-80 Aioi-cho, Naka-ku, Yokohama, 231-0012, Japan.

Bunkei Matsushita (B)

Faculty of Life and Environmental Sciences, University of Tsukuba, 1-1-1 Tennodai, Tsukuba, 305-8572, Japan.

Classifications MeSH