Japan Geoscience Union Meeting 2019

Presentation information

[E] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-HW Hydrology & Water Environment

[A-HW22] Materials transport and nutrient cycles in watersheds; from headwaters to coastal seas

Thu. May 30, 2019 10:45 AM - 12:15 PM 201B (2F)

convener:Masahiro Kobayashi(Forestry and Forest Products Research Institute), Seiko Yoshikawa(Institute for Agro-environmental Sciences, National Agriculture and Food Research Organization), Jun Yasumoto(University of the Ryukyus, Faculty of Agriculuture), Adina Paytan(University of California Santa Cruz), Chairperson:Yasumoto Jun(University of the Ryukyus, Faculty of Agriculuture Department of Regional Agricultural Engineering)

11:15 AM - 11:30 AM

[AHW22-14] Calculation of SS concentration coefficients of river water for each land use by a simple watershed model.

*Seiko Yoshikawa1, Donglai Ma1,2, Tadamasa Saito1,3, Kenji Matsumori4, Yuko Itoh5, Masahiro Kobayashi5 (1.Institute for Agro-environmental Sciences, National Agriculture and Food Research Organization, 2.Graduate Scool, Tsukuba University , 3.Faculty of Agriculture, Ibaraki University , 4.Western Region Agricultural Research Center, National Agriculture and Food Research Organization, 5.Forestry and Forest Products Research Institute)

Keywords:watershed land-use model, SS, concentration coefficient

In recent years, sediment-related disasters are increasing due to intensification and localization of rainfall caused by climate change. Although it is difficult to predict the place and extent of sediment-related disasters, we firstly grasp the average concentrations of sediment discharge in recent years and predict increase and decrease in the sediment concentrations when the way of rain changes. Sediment runoff is depend on land use and land cover, conservative measures, topography, climate condition mainly rainfall etc.. Among them, the land use and land cover is expected to be great in normal climate conditions. Here, in order to contribute to the prediction of sediment-related disasters in the future, coefficients that indicate the SS load intensity to rivers of each land use for the river watersheds across the country are calculated using a simple watershed land use model.
Watersheds whose lower ends are observation points of water quality, and whose land use ratios were determined by GIS technique using published database of DEM (GSI, 10B, raster data) and LULC mesh data (JAXA , ALOS AVNIR-2, 10m mesh data). The SS concentration coefficients of paddy, upland, forest, and urban were calculated by applying the below multiple regression equation using the land use ratios and published SS data( Ministry of Environment).

C = a1 x1+a2 x2+a3 x3 +a4 x4

C: SS concentration (mg L-1) ai : SS concentration coefficient for land use i, xi : ratio of land use i, Land use i : 1;paddy 2;upland fields 3;forest 4;urban

The SS concentration coefficient is 15.4 (lower limit 95% value 12.0 to upper limit 95% value 18.8), 11.5 (7.4 to 15.6), 3.9 (2.6 to 5.1), 11.2 (9.2 to 13.2) for paddy fields, upland fields, forests and urban areas respectively (n=5103).
In order to investigate further in detail, it is necessary to analyze fertilization, soil properties, livestock industry in the watershed, climatic conditions (especially rainfall amount), topographical and geographical features and so on.