Studies on the Groundwater in Alluvium (Ⅱ) On the ... 1欧 χ 「 AjTAipnpuoo oinoaig...

Preview:

Citation preview

  • ()

    Studies on the Groundwater in Alluvium

    On the Increasing Salinity of Groundwater in the Yamaii Area

    at the Lower Basin of Watari River

    Chiaki Agemori, Kunihide Chikamori

    and Seisuke Matsuda

    toft-tilit ,ll iclt

    Yamaji area is situated on the right side at the distances of 5.56.5 km from the estuary of Watari

    River which is discharged into Tosa Bay. And it is small paddy fieldwith about 13 ha. area.

    few years ago, Yamaji River streamed along the south side of thisarea. but now it was digged

    and enlarged for increasing the discharge of Nakasuji River and it was drived to Sanezaki of A'atrai

    River. Recently, tomato and cucumber in this area have been caltivatedingreen house about same

    areas (1. 8 hci).

    The aquifer in this area became contaminated with saltwater during January and February of 1970

    and saltinjury occured. And so, to examine causes an investigation was done by Nakamura office

    of ministry of Construction.

    In this paper, authers obtained the{ollov/ing results by analyzing thesdata, (a) salt water intrudes

    inland through the confined aquifer from Watari River, and (b) the fluctuationof piezometric head

    responds to changes in Nakasuji water level with tides. (c) Salt water intrusion has been accentuated

    by overpumping due to irrigation.

    (Fig. 1), 5.56. 5 km

    13 ha

    J

    Fig. 1. Plain view of lower basinof Watari River

  • 8819

    39

    35441.8

    ha

    45

    Ground EL

    Bor. No 10.986 m.

    _r7

    C

    CDQ

    Q-L1

    |

    a>ex

    (/>

    Loam1.8

    0.7 Clay

    3.1

    Loam

    1.0 Loam

    gravel

    5.84.8

    .:?'.

    ,i.j

    :.0:

    Sandygravel

    7.26.2

    :y..;

    Sandygravel

    9.28.2 2.0

    Sandy

    gravel

    11.2

    10.2 2.0

    9

    Sand

    and

    grave

    13.512.5 2.3

    Sandy

    gravel

    and

    silt

    Ground EL

    Bor. No.20.195 m

    -

    Q.

    Ijj

    Q.Q

    (/1

    3.43.2 3.4

    Clav

    -

    4.03.8 0.6 'j

    6.2

    y

    :'.

    9

    Sandygravel

    6.8 6.6 0.6 rQ Sand

    8.5 2.5

    Sandy .

    gravel

    o. Loam

    10.4

    10.2 1.0

    Fine

    sand

    Ground EL

    Bot. No 33.80 m.

    a

    OJQ

    -

    U

    QjQ

    S

    O

    (/l

    0.8 3.0 0.8 ..ySandgrave!

    610

    5.2

    Clav

    8.85.0 2.8

    Sandy

    silt

    10.3

    6.5 1.5

    o

    1

    Sandy

    gravel

    11.0

    7.2 0.7.

    12.58.7 1.5

    Fine

    sand

    15.011.2 2.5

    Sand

    and

    silt

    19.5

    15.7

    siltv

    clay

    Fig. 2. Geoogical profiles of Yamaji area

  • Si'

Recommended