CConstaterende datVenray
Koppel je AI →
Document · PDF

19 N270 Via Venray Watertoets

Gemeenteraad 14 december 2021, gemeente VenrayBij agendapunt: Bestemmingsplan N270 Via Venray.31.422 woorden

Open het PDF bij de gemeente ↗Naar de vergadering →

Tekst van het document

Uit het bestand gehaald, zonder opmaak, tabellen en afbeeldingen · deel 3 van 3

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 151 (traject 0,5 - 1,5 m-mv) 3de meting

time of discharge

field data

247

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

2360 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

3,9E-5 m 3/s

value "Q"

39,3 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

1,000 m

distance between the water surface in the auger hole and the water table

value "V"

1,19

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

2,3E-5 ONWAAR

if H > 3h then "I" : ground surface

0,07

m

13

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 5,0E-5 WAAR

if h <=H <=3h then "II" :

5,0E-5 ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

1,5

m

water table or impervious layer

equation used is 'II' , as h <=H <= 3h

5,0

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-5

m/s

<=>

180 mm/h

<=>

433,2 cm/day

5,0E-5

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 151 (traject 0,5 - 1,5 m-mv) 4de meting

time of discharge

field data

243

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

2328 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

3,9E-5 m 3/s

value "Q"

38,8 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

1,000 m

distance between the water surface in the auger hole and the water table

value "V"

1,19

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

2,3E-5 ONWAAR

if H > 3h then "I" : ground surface

0,07

m

13

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 4,9E-5 WAAR

if h <=H <=3h then "II" :

4,9E-5 ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

1,5

m

water table or impervious layer

equation used is 'II' , as h <=H <= 3h

4,9

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-5

m/s

<=>

178 mm/h

<=>

427,2 cm/day

4,9E-5

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 201 (traject 0,5 - 1,5 m-mv) 1ste meting

time of discharge

field data

75

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

718 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

1,2E-5 m 3/s

value "Q"

12,0 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

1,000 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

7,2E-6 ONWAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 1,6E-5 WAAR

if h <=H <=3h then "II" :

1,6E-5 ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

1,5

m

water table or impervious layer

equation used is 'II' , as h <=H <= 3h

1,6

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-5

m/s

<=>

56 mm/h

<=>

135,3 cm/day

1,6E-5

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 201 (traject 0,5 - 1,5 m-mv) 2de meting

time of discharge

field data

84

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

808 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

1,3E-5 m 3/s

value "Q"

13,5 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

1,000 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

8,1E-6 ONWAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 1,8E-5 WAAR

if h <=H <=3h then "II" :

1,8E-5 ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

1,5

m

water table or impervious layer

equation used is 'II' , as h <=H <= 3h

1,8

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-5

m/s

<=>

63 mm/h

<=>

152,2 cm/day

1,8E-5

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 201 (traject 0,5 - 1,5 m-mv) 3de meting

time of discharge

field data

84

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

801 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

1,3E-5 m 3/s

value "Q"

13,3 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

1,000 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

8,0E-6 ONWAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 1,7E-5 WAAR

if h <=H <=3h then "II" :

1,7E-5 ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

1,5

m

water table or impervious layer

equation used is 'II' , as h <=H <= 3h

1,7

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-5

m/s

<=>

63 mm/h

<=>

151,0 cm/day

1,7E-5

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 204 (traject 0,5 - 1,5 m-mv) 1ste meting

time of discharge

field data

141

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

1346 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

2,2E-5 m 3/s

value "Q"

22,4 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

1,000 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

1,3E-5 ONWAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 2,9E-5 WAAR

if h <=H <=3h then "II" :

2,9E-5 ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

1,5

m

water table or impervious layer

equation used is 'II' , as h <=H <= 3h

2,9

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-5

m/s

<=>

106 mm/h

<=>

253,8 cm/day

2,9E-5

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 204 (traject 0,5 - 1,5 m-mv) 2de meting

time of discharge

field data

160

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

1535 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

2,6E-5 m 3/s

value "Q"

25,6 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

1,000 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

1,5E-5 ONWAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 3,3E-5 WAAR

if h <=H <=3h then "II" :

3,3E-5 ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

1,5

m

water table or impervious layer

equation used is 'II' , as h <=H <= 3h

3,3

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-5

m/s

<=>

121 mm/h

<=>

289,3 cm/day

3,3E-5

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 204 (traject 0,5 - 1,5 m-mv) 3de meting

time of discharge

field data

194

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

1851 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

3,1E-5 m 3/s

value "Q"

30,9 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

1,000 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

1,9E-5 ONWAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 4,0E-5 WAAR

if h <=H <=3h then "II" :

4,0E-5 ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

1,5

m

water table or impervious layer

equation used is 'II' , as h <=H <= 3h

4,0

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-5

m/s

<=>

145 mm/h

<=>

349,0 cm/day

4,0E-5

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 204 (traject 0,5 - 1,5 m-mv) 4de meting

time of discharge

field data

217

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

2076 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

3,5E-5 m 3/s

value "Q"

34,6 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

1,000 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

2,1E-5 ONWAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 4,5E-5 WAAR

if h <=H <=3h then "II" :

4,5E-5 ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

1,5

m

water table or impervious layer

equation used is 'II' , as h <=H <= 3h

4,5

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-5

m/s

<=>

163 mm/h

<=>

391,4 cm/day

4,5E-5

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 204 (traject 0,5 - 1,5 m-mv) 5de meting

time of discharge

field data

212

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

2024 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

3,4E-5 m 3/s

value "Q"

33,7 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

1,000 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

2,0E-5 ONWAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 4,4E-5 WAAR

if h <=H <=3h then "II" :

4,4E-5 ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

1,5

m

water table or impervious layer

equation used is 'II' , as h <=H <= 3h

4,4

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-5

m/s

<=>

159 mm/h

<=>

381,5 cm/day

4,4E-5

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 206 (traject 0,5 - 1,5 m-mv) 2de meting

time of discharge

60 sec

value "Q"

2,3 ml/s

field data

15

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

140 ml (Durchm.Messzyl:

110,4

mm)

2,3E-6 m 3/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

1,000 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

1,4E-6 ONWAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 3,1E-6 WAAR

if h <=H <=3h then "II" :

3,1E-6 ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

1,5

m

water table or impervious layer

equation used is 'II' , as h <=H <= 3h

3,1

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-6

m/s

<=>

11 mm/h

<=>

26,5 cm/day

3,1E-6

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 209 (traject 0,5 - 1,5 m-mv) 1ste meting

time of discharge

field data

191

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

1823 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

3,0E-5 m 3/s

value "Q"

30,4 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

4,500 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

1,8E-5 WAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 1,2E-5 ONWAAR

if h <=H <=3h then "II" :

--ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

5,0

m

water table or impervious layer

equation used is 'I' as H > 3h

1,8

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-5

m/s

<=>

66 mm/h

<=>

157,9 cm/day

1,8E-5

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 209 (traject 0,5 - 1,5 m-mv) 2de meting

time of discharge

field data

173

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

1653 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

2,8E-5 m 3/s

value "Q"

27,6 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

4,500 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

1,7E-5 WAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 1,1E-5 ONWAAR

if h <=H <=3h then "II" :

--ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

5,0

m

water table or impervious layer

equation used is 'I' as H > 3h

1,7

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-5

m/s

<=>

60 mm/h

<=>

143,2 cm/day

1,7E-5

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 209 (traject 0,5 - 1,5 m-mv) 3de meting

time of discharge

field data

164

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

1569 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

2,6E-5 m 3/s

value "Q"

26,2 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

4,500 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

1,6E-5 WAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 1,0E-5 ONWAAR

if h <=H <=3h then "II" :

--ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

5,0

m

water table or impervious layer

equation used is 'I' as H > 3h

1,6

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-5

m/s

<=>

57 mm/h

<=>

135,9 cm/day

1,6E-5

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 209 (traject 0,5 - 1,5 m-mv) 4de meting

time of discharge

field data

153

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

1464 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

2,4E-5 m 3/s

value "Q"

24,4 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

4,500 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

1,5E-5 WAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 9,6E-6 ONWAAR

if h <=H <=3h then "II" :

--ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

5,0

m

water table or impervious layer

equation used is 'I' as H > 3h

1,5

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-5

m/s

<=>

53 mm/h

<=>

126,8 cm/day

1,5E-5

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 211 (traject 0,5 - 1,5 m-mv) 1ste meting

time of discharge

60 sec

value "Q"

6,6 ml/s

field data

41

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

397 ml (Durchm.Messzyl:

110,4

mm)

6,6E-6 m 3/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

4,500 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

4,0E-6 WAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 2,6E-6 ONWAAR

if h <=H <=3h then "II" :

--ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

5,0

m

water table or impervious layer

equation used is 'I' as H > 3h

4,0

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-6

m/s

<=>

14 mm/h

<=>

34,4 cm/day

4,0E-6

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 211 (traject 0,5 - 1,5 m-mv) 2de meting

time of discharge

60 sec

value "Q"

6,2 ml/s

field data

39

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

373 ml (Durchm.Messzyl:

110,4

mm)

6,2E-6 m 3/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

4,500 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

3,7E-6 WAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 2,4E-6 ONWAAR

if h <=H <=3h then "II" :

--ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

5,0

m

water table or impervious layer

equation used is 'I' as H > 3h

3,7

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-6

m/s

<=>

13 mm/h

<=>

32,3 cm/day

3,7E-6

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 212 (traject 0,5 - 1,5 m-mv) 1ste meting

time of discharge

60 sec

value "Q"

9,6 ml/s

field data

60

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

578 ml (Durchm.Messzyl:

110,4

mm)

9,6E-6 m 3/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

4,500 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

5,8E-6 WAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 3,8E-6 ONWAAR

if h <=H <=3h then "II" :

--ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

5,0

m

water table or impervious layer

equation used is 'I' as H > 3h

5,8

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-6

m/s

<=>

21 mm/h

<=>

50,1 cm/day

5,8E-6

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 212 (traject 0,5 - 1,5 m-mv) 2de meting

time of discharge

field data

73

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

700 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

1,2E-5 m 3/s

value "Q"

11,7 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

4,500 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

7,0E-6 WAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 4,6E-6 ONWAAR

if h <=H <=3h then "II" :

--ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

5,0

m

water table or impervious layer

equation used is 'I' as H > 3h

7,0

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-6

m/s

<=>

25 mm/h

<=>

60,7 cm/day

7,0E-6

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 212 (traject 0,5 - 1,5 m-mv) 3de meting

time of discharge

field data

83

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

789 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

1,3E-5 m 3/s

value "Q"

13,2 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

4,500 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

7,9E-6 WAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 5,2E-6 ONWAAR

if h <=H <=3h then "II" :

--ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

5,0

m

water table or impervious layer

equation used is 'I' as H > 3h

7,9

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-6

m/s

<=>

28 mm/h

<=>

68,4 cm/day

7,9E-6

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 213 (traject 0,5 - 1,5 m-mv) 1ste meting

time of discharge

60 sec

value "Q"

9,2 ml/s

field data

58

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

550 ml (Durchm.Messzyl:

110,4

mm)

9,2E-6 m 3/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

1,000 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

5,5E-6 ONWAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 1,2E-5 WAAR

if h <=H <=3h then "II" :

1,2E-5 ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

1,5

m

water table or impervious layer

equation used is 'II' , as h <=H <= 3h

1,2

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-5

m/s

<=>

43 mm/h

<=>

103,7 cm/day

1,2E-5

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 213 (traject 0,5 - 1,5 m-mv) 2de meting

time of discharge

field data

64

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

609 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

1,0E-5 m 3/s

value "Q"

10,2 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

1,000 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

6,1E-6 ONWAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 1,3E-5 WAAR

if h <=H <=3h then "II" :

1,3E-5 ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

1,5

m

water table or impervious layer

equation used is 'II' , as h <=H <= 3h

1,3

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-5

m/s

<=>

48 mm/h

<=>

114,9 cm/day

1,3E-5

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 213 (traject 0,5 - 1,5 m-mv) 3de meting

time of discharge

field data

63

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

605 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

1,0E-5 m 3/s

value "Q"

10,1 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

1,000 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

6,1E-6 ONWAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 1,3E-5 WAAR

if h <=H <=3h then "II" :

1,3E-5 ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

1,5

m

water table or impervious layer

equation used is 'II' , as h <=H <= 3h

1,3

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-5

m/s

<=>

48 mm/h

<=>

114,0 cm/day

1,3E-5

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 216 (traject 0,5 - 1,5 m-mv) 1ste meting

time of discharge

field data

197

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

1880 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

3,1E-5 m 3/s

value "Q"

31,3 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

1,000 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

1,9E-5 ONWAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 4,1E-5 WAAR

if h <=H <=3h then "II" :

4,1E-5 ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

1,5

m

water table or impervious layer

equation used is 'II' , as h <=H <= 3h

4,1

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-5

m/s

<=>

148 mm/h

<=>

354,5 cm/day

4,1E-5

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

FIELD PERMEABILITY TESTING BOREHOLE PERMEAMETER METHOD field data

calculations interim results

Projectnaam: N270 Via Venray

flow of water

Projectnummer: 417318 Boring: 216 (traject 0,5 - 1,5 m-mv) 2de meting

time of discharge

field data

213

mm water flow per interval (1mm ~ 10 ml)

1

min final time interval

2041 ml 60 sec

(Durchm.Messzyl:

110,4

mm)

3,4E-5 m 3/s

value "Q"

34,0 ml/s

rate of infiltration

value "r"

0,035 m

effective radius of well

value "h"

1,000 m

height of water in auger hole

value "H"

1,000 m

distance between the water surface in the auger hole and the water table

value "V"

1,23

viscosity of water in auger hole o

viscositiy at 20 C conditions I, II, III *)

equations: I, II, III *)

2,0E-5 ONWAAR

if H > 3h then "I" : ground surface

0,07

m

12

o

C

temperature of water

1,0

m

height of water in auger hole

diameter of auger hole 4,5E-5 WAAR

if h <=H <=3h then "II" :

4,5E-5 ONWAAR

if H < h then "III" :

1,5

m

depth auger hole

1,5

m

water table or impervious layer

equation used is 'II' , as h <=H <= 3h

4,5

coefficient k20

Copyright 2001-2009 H.H.Wiltschut

* 10

-5

m/s

<=>

160 mm/h

<=>

384,8 cm/day

4,5E-5

*) U.S.Department of the Interior: EARTH MANUAL Part 2, Third Edition, P.1234-5. Denver, Colorado 1990.

De tekst is automatisch uit het bestand gehaald en kan afwijken van het origineel (kolommen, tabellen en koppen lopen door elkaar). Het officiële stuk bij de gemeente is leidend. Bron: https://api.notubiz.nl/document/10736241/1