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Multiple-indicator study of the response of groundwater recharge sources to highly turbid river water after a landslide in the Tedori River alluvial fan, Japan

Yoshioka Yumi Nakamura Kimihito Takimoto Hiroshi Sakurai Shinji Nakagiri Takao Horino Haruhiko Tsuchihara Takeo 大阪府立大学

2020.08.25

概要

Groundwater recharge is a key process in regional water cycles. The large volume of groundwater stored in
the Tedori River alluvial fan of Ishikawa Prefecture, Japan, is a crucial drinking and industrial water resource.
Paddy fields occupy about 50% of the land surface area of the alluvial fan (National Land Numerical
Information download service, 2014), and irrigation water in the paddy fields is considered to be one of the
major groundwater recharge sources, in addition to other surface water runoff (Iwasaki et al., 2014; Yoshioka
et al., 2016). The water in the Tedori River was observed to be highly turbid from the beginning of May 2015
to at least November 2017 due to a large landslide that occurred in the upper reaches of the river in May 2015.
Indeed, the volume of landslide deposits in 2015 was 1.3 million m3 (Yanai et al., 2016b). In the fan, the
groundwater level was drawn down by several to ten meters during the 2015 irrigation period, and this
drawdown trend persisted during the 2016 irrigation period (Yoshioka et al., 2018). The highly turbid river
water caused siltation, and may have reduced groundwater recharge from the river or paddy fields because
the irrigation water is derived from the river. ...

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Figure 1. Maps showing (a) the regional location of the Tedori River basin, and (b) the Tedori River basin

watershed and the neighboring Sai and Kakehashi River basins. Red rectangle in (b) delineates the area of

the Tedori River alluvial fan.

24

Figure 2. Detailed maps of the study area showing (a) surface geology (modified from the Geological Survey

of Japan, 2015), (b) land use conditions in 2014 (data from the National Land Numerical Information

download service, 2014), (c) irrigation channel, and (d) contours of surface and groundwater levels and river

sections of groundwater - river water interactions.

25

Figure 3. Temporal variations of (a) monthly precipitation (gray bar) and annual precipitation (black dash

line), (b) Tedori River water turbidity, (c) river discharge (blue curve) and daily precipitation (black bar), (d)(f) groundwater levels along the left (red curve) and right banks (blue curve).

26

Figure 4. Detailed maps of the study area showing (a) sampling sites of groundwater and (b) sampling sites

of surface water.

Note: 1, 7, 18, 19 sites are not shown and data are unavailable.

27

Figure 5. Distribution of TN concentrations (grey scale) and hexadiagrams indicating dissolved ion

concentrations in groundwater in (a) June 2011 and (b) June 2016. Hexadiagram symbol colors indicate the

zone of the study area (see Figure 4a).

28

Figure 6. Comparison of dissolved ion concentrations, TN, oxygen isotopic compositions, and Sr isotopic

ratios between June 2011 and June 2016.

29

Figure 7. Box plots of chemical and isotopic groundwater components from (a) zone I, the left bank of the

Tedori River, (b) zone II, the right bank area near the Tedori River, (c) zones III and IV, the right bank area

farther from the river, and (d) and river waters from the Tedori, Sai, and Kakehashi Rivers. Horizontal lines

in the boxes show the median values, the boxes encompass the second and third quartiles, and whiskers show

maximum and minimum values.

30

Figure 8. 87Sr/86Sr ratios of Tedori (RT-), Sai (RS-), Kakehashi (RK-) River waters and precipitation.

31

Figure 9. Distribution of shallow groundwater

87Sr/86Sr

ratios (circles and background interpolated color

map) in the study site in (a) June 2011 and (b) June 2016. The

87Sr/86Sr

ratios of river waters and paddy

ponding waters are shown as triangles and rectangles for comparison (see Figure 4 and d for symbols).

32

Figure 10. Groundwater (circles) and surface water 87Sr/86Sr ratios vs the reciprocal of Sr concentration in

(a) June 2011 and (b) April, (c) June, (d) August, (e) October, (f) December 2016, and (g) all sampling periods

and the conceptural models. Red cross shows mixing rate with 20% increments in each survey time. Twoendmember mixing areas between average values of all the Tedori River water (100%) and three groundwater

samples in zone III (0%) are shown in 20% increments by the light to dark gray shaded areas. See text for

details of the mixing model. Overlapping mixing areas are not shaded.

33

Figure 11. Comparison of mixing ratios of the Tedori River water between end member mixing analysis using

δ18O and δD (Tsuchihara et al., 2011) and

87Sr/86Sr

Figures represent the sampling location (see Figure 3).

34

and Sr concentration (this study). Numbers in the

Figure 12. Mixing ratios of Tedori River water to zone III/IV groundwater (percent) in (a) June 2011 and

(b) April, (c) June, (d) August, (e) October, and (f) December 2016. Black symbols plotted outside of the

mixing areas in Figure 10, and were assigned mixing ratios of zero.

Data Availability Statement

Data available on request due to privacy/ethical restrictions

35

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