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Materials and Geoenvironment
Volume 66 (2019): Issue 4 (December 2019)
Open Access
Spatial Resistivity Mapping of Ureje Dam Floor, Southwestern Nigeria
J.O. Fatoba
J.O. Fatoba
,
A.B. Eluwole
A.B. Eluwole
,
O.A. Sanuade
O.A. Sanuade
and
M.T. Aroyehun
M.T. Aroyehun
| Jun 15, 2020
Materials and Geoenvironment
Volume 66 (2019): Issue 4 (December 2019)
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Article Category:
Original scientific paper
Published Online:
Jun 15, 2020
Page range:
245 - 255
Received:
Jun 22, 2019
Accepted:
Dec 18, 2019
DOI:
https://doi.org/10.2478/rmzmag-2019-0025
Keywords
Drastic reduction
,
vulnerability
,
spatial demarcation
,
impounded water
© 2019 Fatoba J.O. et al., published by Sciendo
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.
Figure 1
Location Map of the Study Area.
Figure 2
Geological Map of the Area Around Ado-Ekiti Showing the Ureje Dam site (After [20]).
Figure 3
Geophysical Data Acquisition Map.
Figure 4
Typical Depth Sounding Curves. (a) A – Type, (b) K – Type, (c) KH – Type and (d) KHA – Type.
Figure 5
Geoelectric Sections Beneath the Dam Floor (a) Section A – B (b) Section C – D, (c) Section E – F.
Figure 6
Spatial Vulnerability Assessment from Thickness of Suspended Materials.
Figure 7
Spatial Vulnerability Assessment from Resistivity of Weathered Layer.
Figure 8
Spatial Vulnerability Assessment from Presence of Near-surface Clay Substratum.
Figure 9
Cumulative Spatial Vulnerability Map.
Colour Chart of the Distribution of the Depth Sounding Curves.
VES LOCATIONS
KEY
1
10
19
p
1
>
p
2
>
p
3
= A-Type Curve
2
11
20
p
1
〈
p
2
〉
p
3
= K-Type Curve
3
12
21
p
1
〈
p
2
〉
p
3
p
4
= KH-Type Curve
4
13
22
p
1
〈
p
2
〉
p
3
<
p
4
<
p
5
= KHA-Type Curve
5
14
23
6
15
24
7
16
25
8
17
9
18