NUTRIENT RUNOFF IN THE KAMAFUSA CATCHMENT

In the Kamafusa Lake catchment, we measured water discharge and water samples once a month at twelve points and once an hour at one point. The samples were analyzed for total-phosphrus, souble-P, total-N, nitrate-nitrogen, and ammonium-nitrogen. In a flood, the increasin g of total-N is similar to w...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:PROCEEDINGS OF HYDRAULIC ENGINEERING 2002/02/10, Vol.46, pp.223-228
Hauptverfasser: KATAYAMA, Seiichiro, KAZAMA, So, SU, Baolin, SAWAMOTO, Masaki
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:In the Kamafusa Lake catchment, we measured water discharge and water samples once a month at twelve points and once an hour at one point. The samples were analyzed for total-phosphrus, souble-P, total-N, nitrate-nitrogen, and ammonium-nitrogen. In a flood, the increasin g of total-N is similar to water discharge, and the increasing of total-P is earlier than the increasing of water discharge. Inorganic nitrogen is almost covered with nitrate-nitrogen in this catchment. The upper-course in forest, nitrogen runoff is larger but middle-course is smaller, and downstream is large. The reason is why upper-course covered with forest land, in middle-course has smaller forest is decreasing, and downstream has urban field usually. Nitrogen flow out from urban area in this area. On the other hand, Nitrogen flow out from urban area, barron land and paddy field in flood period.
ISSN:0916-7374
1884-9172
DOI:10.2208/prohe.46.223