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Silting of Togo inshore sedimentary basin rivers and protection measures: Case of Zio river

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par Akintola S. Nelson AKIBODE
Technische Universität Dresden/Germany (CIPSEM Centre for International Postgraduate Studies in Environmental Management) - Diploma of Environmental Management 2007
  

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2.4.2 Zio Hydrological assessment

Zio takes its source in the dorsal of Atakora whose extension in latitude prolongs in soudanian zone which records 1500 mm per year, characteristic of Guinean wet climate. This dorsal thanks to the impermeability of its substratum schist quartzitic, the river maintains a area flow to 30 m3/s in periods of high waters. Other hand, in the more permeable sedimentary basin where average rainy is 1000 mm in seasons of strong rains, the flow is lower than 10 m3/s.

The years of low water level record severe about 1.4 m3/s or sometimes null flows when the year is very dry. This deficit includes all water losses due to evaporation, evapotranspiration, and infiltration. The report, ratio flow of flood/minimum flow and the flow coefficients which are indicators of checking evolution and importance of past water remain in together weak for the Zio river because clays abundance and very permeable alluvia. Direct consequence of flow deficit is the small quantity of the past water blades; table (6) presents the coefficients of Zio flow over 20 years period.

Total rain amounts explain well the interannual variations of the flow coefficients. It is thus advisable to specify that the distribution of rains during year intervenes in the determination of the hydrological mode of the river whose impacts appear through erosion.

Table 6: Calculated values of the Zio flow coefficients

Flow Coefficients (%)

 

years

Kati

Kpédji

Togblé

1980

11,1

9,2

8,8

1981

11,6

11,9

9,1

1982

14,3

20,8

12,7

1983

11,5

10,9

6,6

1984

11,1

4,7

6,1

1985

11,2

9,5

6,8

1986

8,9

6

6

1987

11,3

7,2

9,2

1988

10,8

7,9

7,7

1989

13

10,1

8,8

1990

10,9

5,7

4

1991

6,0

2,7

2

1992

11,2

5,3

5

1993

12,9

16,2

9,5

1994

12,8

16,3

8,5

1995

10

8,4

8,5

1996

10,4

4,4

5

1997

11,7

0,6

1,3

1998

10,8

12,6

10,5

1999

11,1

13,1

7

 

Source: Service Hydrologie-Lomé

 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 

15

 
 
 
 

Kati

 
 

15

 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 

10

 
 
 
 
 
 

10

 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 

5

 
 
 
 
 
 
 
 
 

5

 
 
 
 
 
 

0

 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 

3

5

7

9 1 1 13

1 5

1 7 19 21

 

0

1 3

5

7

91113151719

 
 
 
 
 
 
 

An née s

 
 
 
 
 
 
 

Année s

 
 

Kati

 
 
 

Kpédji

 

Togblé

 
 
 
 
 
 
 
 
 
 
 
 
 

Figure 8:Curves of annual medium flows Figure 9:Curves of evolution of the flow

Zio river over one 20 years period of Zio over 21 years

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