19
Chapter 3 Results and Discussion 3.1 Temporal Development of Horizontal Vortices The development of horizontal vortices can be described by using numerical computation as follow: a. Velocity and vorciticy field as shown in figure 3.2 and 3.3, respectively, at several times, , , , , and , indicating that small scale horizontal vortices appear first and they grow by merging with each other. In the beginning flow, appears weak flow with the corresponding accumulation of vortices in five regions. After t = 90 s, the spatial pattern of velocity and vorticity has been found to reach an equilibrium state which the two large vortices formed. b. The longitudinal wavelength of vortices varies between 60 cm and 110 cm in statistical equilibrium. c. The value of the wavelength both experiment and simulation are shown in table 3.1. The mean value of the wavelength of the vortices predicted (simulation) at the observation point is 61.4 cm. The corresponding length was 58.6, which agrees with the prediction. The calculation for finding the time period (T) of the 32

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Page 1: Flow, Sediment, and Nutrient Transport in a Riparian Mangrove€¦  · Web viewIn the beginning flow, appears weak flow with the corresponding accumulation of vortices in five regions

Chapter 3

Results and Discussion

3.1 Temporal Development of Horizontal Vortices

The development of horizontal vortices can be described by using numerical computation

as follow:

a. Velocity and vorciticy field as shown in figure 3.2 and 3.3, respectively, at several

times, , , , , and , indicating that

small scale horizontal vortices appear first and they grow by merging with each

other. In the beginning flow, appears weak flow with the corresponding

accumulation of vortices in five regions. After t = 90 s, the spatial pattern of

velocity and vorticity has been found to reach an equilibrium state which the two

large vortices formed.

b. The longitudinal wavelength of vortices varies between 60 cm and 110 cm in

statistical equilibrium.

c. The value of the wavelength both experiment and simulation are shown in table

3.1. The mean value of the wavelength of the vortices predicted (simulation) at the

observation point is 61.4 cm. The corresponding length was 58.6, which agrees

with the prediction. The calculation for finding the time period (T) of the

wavelength is done with Fast Fourier Transform (FFT). The result of spectrum

graph is depicted in figure 3.3.

d. Figure 3.5 and 3.6 give comparison which it is found that the regions with water

surface depression nearly coincide with the central parts of horizontal vortices.

Table 3. 1 Comparison value of wavelength ( ).

u (cm/s) Re Froude T (s) λ measured (cm)Simulation 23.9675 14381 0.312 2.56 61.4Measured 20.55 12330 0.268 2.85 58.6

32

Page 2: Flow, Sediment, and Nutrient Transport in a Riparian Mangrove€¦  · Web viewIn the beginning flow, appears weak flow with the corresponding accumulation of vortices in five regions

CHAPTER 3 RESULTS AND DISCUSSION

-0.3

-0.2

-0.1

0

0.1

0.2

0.3

0 10 20 30 40 50 60 70 80 90 100 110 120 130 140 150

Time (sec)

h (m

m)

Figure 3. 1 Variation of water surface elevation at measurement point (numerical calculation)

0

20

40

60

80

100

120

140

0 10 20 30 40 50 60 70 80 90 100 110 120 130 140 150

Time (sec)

l (c

m)

Figure 3. 2 Variation of wave length at measurement point (numerical calculation)

33

Page 3: Flow, Sediment, and Nutrient Transport in a Riparian Mangrove€¦  · Web viewIn the beginning flow, appears weak flow with the corresponding accumulation of vortices in five regions

CHAPTER 3 RESULTS AND DISCUSSION

Figure 3. 3 Result of FFT

34

Page 4: Flow, Sediment, and Nutrient Transport in a Riparian Mangrove€¦  · Web viewIn the beginning flow, appears weak flow with the corresponding accumulation of vortices in five regions

CHAPTER 3 RESULTS AND DISCUSSION

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 20

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

0.3m/secFlow

Frame 001 25 Aug 2006 Vector

(a) t = 10 s

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 20

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

0.3m/secFlow

Frame 001 25 Aug 2006 Vector

(b) t = 30 sFigure 3. 4 Temporal development of horizontal vortices; Spatial distribution velocity at (a) t=10 sec, (b) t = 30 s.

35

Page 5: Flow, Sediment, and Nutrient Transport in a Riparian Mangrove€¦  · Web viewIn the beginning flow, appears weak flow with the corresponding accumulation of vortices in five regions

CHAPTER 3 RESULTS AND DISCUSSION

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 20

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

0.3m/secFlow

Frame 001 25 Aug 2006 Vector

(c) t = 60 s

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 20

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

0.3m/secFlow

Frame 001 25 Aug 2006 Vector

(d) t = 90 sFigure 3.4 Temporal development of horizontal vortices; Spatial distribution velocity at (c) t=60 sec, (d) t = 90 s (continued).

36

Page 6: Flow, Sediment, and Nutrient Transport in a Riparian Mangrove€¦  · Web viewIn the beginning flow, appears weak flow with the corresponding accumulation of vortices in five regions

CHAPTER 3 RESULTS AND DISCUSSION

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 20

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

0.3m/secFlow

Frame 001 25 Aug 2006 Vector

(e) t = 120 s

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 20

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

0.3m/secFlow

Frame 001 25 Aug 2006 Vector

(f) t = 150 sFigure 3.4 Temporal development of horizontal vortices; Spatial distribution velocity at (e) t=120 sec, (f) t = 150 s (continued).

37

Page 7: Flow, Sediment, and Nutrient Transport in a Riparian Mangrove€¦  · Web viewIn the beginning flow, appears weak flow with the corresponding accumulation of vortices in five regions

CHAPTER 3 RESULTS AND DISCUSSION

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 2

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

vor: -4.5 -4 -3.5 -3 -2.5 -2 -1.5 -1 -0.5Flow

Frame 001 25 Aug 2006 Vector

(a) t = 10 s

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 2

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

vor: -4.5 -4 -3.5 -3 -2.5 -2 -1.5 -1 -0.5Flow

Frame 001 25 Aug 2006 Vector

(b) t = 30 sFigure 3. 5 Temporal development of horizontal vortices; Spatial distribution vorticity at (a) t=10 sec, (b) t = 30 s.

38

Page 8: Flow, Sediment, and Nutrient Transport in a Riparian Mangrove€¦  · Web viewIn the beginning flow, appears weak flow with the corresponding accumulation of vortices in five regions

CHAPTER 3 RESULTS AND DISCUSSION

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 2

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

vor: -4.5 -4 -3.5 -3 -2.5 -2 -1.5 -1 -0.5Flow

Frame 001 25 Aug 2006 Vector

(c) t = 60 s

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 2

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

vor: -4.5 -4 -3.5 -3 -2.5 -2 -1.5 -1 -0.5Flow

Frame 001 25 Aug 2006 Vector

(d) t = 90 sFigure 3.5 Temporal development of horizontal vortices; Spatial distribution vorticity at (c) t=60 sec, (d) t = 90 s (continued).

39

Page 9: Flow, Sediment, and Nutrient Transport in a Riparian Mangrove€¦  · Web viewIn the beginning flow, appears weak flow with the corresponding accumulation of vortices in five regions

CHAPTER 3 RESULTS AND DISCUSSION

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 2

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

vor: -4.5 -4 -3.5 -3 -2.5 -2 -1.5 -1 -0.5Flow

Frame 001 25 Aug 2006 Vector

(e) t = 120 s

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 2

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

vor: -4.5 -4 -3.5 -3 -2.5 -2 -1.5 -1 -0.5Flow

Frame 001 25 Aug 2006 Vector

(f) t = 150 sFigure 3.5 Temporal development of horizontal vortices; Spatial distribution vorticity at (c) t=120 sec, (d) t = 150 s (continued).

40

Page 10: Flow, Sediment, and Nutrient Transport in a Riparian Mangrove€¦  · Web viewIn the beginning flow, appears weak flow with the corresponding accumulation of vortices in five regions

CHAPTER 3 RESULTS AND DISCUSSION

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 20

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

eta: -0.00016m -0.00012m -8E-05m -4E-05m -8.13152E-20m 4E-05m 8E-05m 0.00012mFlow

Frame 001 14 Sep 2006 Vector

(a) t = 10 s

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 20

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

eta: -0.00016m -0.00012m -8E-05m -4E-05m -8.13152E-20m 4E-05m 8E-05m 0.00012mFlow

Frame 001 14 Sep 2006 Vector

(b) t = 30 sFigure 3. 6 Temporal development of horizontal vortices; spatial distribution water surface at (a) t=10 sec, (b) t = 30 s.

41

Page 11: Flow, Sediment, and Nutrient Transport in a Riparian Mangrove€¦  · Web viewIn the beginning flow, appears weak flow with the corresponding accumulation of vortices in five regions

CHAPTER 3 RESULTS AND DISCUSSION

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 20

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

eta: -0.00016m -0.00012m -8E-05m -4E-05m -8.13152E-20m 4E-05m 8E-05m 0.00012mFlow

Frame 001 14 Sep 2006 Vector

(c) t = 60 s

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 20

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

eta: -0.00016m -0.00012m -8E-05m -4E-05m -8.13152E-20m 4E-05m 8E-05m 0.00012mFlow

Frame 001 14 Sep 2006 Vector

(d) t = 90 sFigure 3.6 Temporal development of horizontal vortices; spatial distribution water surface at (c) t=60 sec, (d) t = 90 s (continued).

42

Page 12: Flow, Sediment, and Nutrient Transport in a Riparian Mangrove€¦  · Web viewIn the beginning flow, appears weak flow with the corresponding accumulation of vortices in five regions

CHAPTER 3 RESULTS AND DISCUSSION

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 20

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

eta: -0.00016m -0.00012m -8E-05m -4E-05m -8.13152E-20m 4E-05m 8E-05m 0.00012mFlow

Frame 001 14 Sep 2006 Vector

(e) t = 120 s

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 20

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

eta: -0.00016m -0.00012m -8E-05m -4E-05m -8.13152E-20m 4E-05m 8E-05m 0.00012mFlow

Frame 001 14 Sep 2006 Vector

(f) t = 150 sFigure 3.6 Temporal development of horizontal vortices; spatial distribution water surface at (e) t=120 sec, (f) t = 150 s (continued).

43

Page 13: Flow, Sediment, and Nutrient Transport in a Riparian Mangrove€¦  · Web viewIn the beginning flow, appears weak flow with the corresponding accumulation of vortices in five regions

CHAPTER 3 RESULTS AND DISCUSSION

3.2 Instantaneous Flow Field

The instantaneous 2D velocity with water surface contour and vorticity field are depicted

in figure 3.5 and 3.6, respectively, in which the velocity field is seen in the frame moving

with the temporally averaged velocity at the boundary of the main channel and the flood

channel (y = 16 cm). The maximum vorticity locates upstream of the geometrical center of

the vortex. The vortices are inclined toward the longitudinal direction, which is important

in producing the Reynolds stress.

The instantaneous free surface elevation calculated is shown in Figure 3.4, in which it is

clear that the elevation is low near the center of the vortices. The variations of free surface

elevation at y = 16 cm are depicted in figure 3.7 and 3.8 for the measurement and

prediction, respectively. In the measurement graph, the form is quite different with the

prediction, but the range of the variation of height water surface and time period are

similar. The calculation of period time gives the same result.

44

Page 14: Flow, Sediment, and Nutrient Transport in a Riparian Mangrove€¦  · Web viewIn the beginning flow, appears weak flow with the corresponding accumulation of vortices in five regions

CHAPTER 3 RESULTS AND DISCUSSION

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 2

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

eta: -0.00016m -0.00012m -8E-05m -4E-05m -8.13152E-20m 4E-05m 8E-05m 0.00012m0.3 m/secFlow

Frame 001 14 Sep 2006 Velocity

Figure 3. 7 2D velocity with water surface contour.

x (m)

y(m

)

0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 2

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

1.3

1.4

1.5

1.6

1.7

1.8

vor: -4.5 -4 -3.5 -3 -2.5 -2 -1.5 -1 -0.50.3 m/secFlow

Frame 001 25 Aug 2006 Velocity

Figure 3. 8 2D velocity with vorticity contour.

45

Page 15: Flow, Sediment, and Nutrient Transport in a Riparian Mangrove€¦  · Web viewIn the beginning flow, appears weak flow with the corresponding accumulation of vortices in five regions

CHAPTER 3 RESULTS AND DISCUSSION

Figure 3. 9 Temporal variation of free surface (measured).

Figure 3. 10 Calculated variation of free surface.

3.3 Temporally-averaged Flow Field

The lateral velocity distribution is shown in figure 3.9 The agreement is reasonable.

However, the measured values near y = 17 cm are a little smaller than the prediction, the

reason for which is the existence of secondary flow which is fairly large near the boundary

of the main channel and the flood plain. It transports near-bottom small fluid momentum

toward the free surface, inducing small longitudinal flow velocity at around y = 20 cm. The

present model cannot include the effect of secondary flow.

46

Page 16: Flow, Sediment, and Nutrient Transport in a Riparian Mangrove€¦  · Web viewIn the beginning flow, appears weak flow with the corresponding accumulation of vortices in five regions

CHAPTER 3 RESULT AND DISCUSSION

0

5

10

15

20

25

30

35

40

45

50

00.050.10.150.20.250.30.350.4

y (cm)

(cm

/sec

)

ExperimentNumerical Simulation

u

Figure 3. 11 Transverse profiles of mean velocity.

47

(cm/s)

Page 17: Flow, Sediment, and Nutrient Transport in a Riparian Mangrove€¦  · Web viewIn the beginning flow, appears weak flow with the corresponding accumulation of vortices in five regions

CHAPTER 3 RESULT AND DISCUSSION

Chapter 3..............................................................................................................................32

Result and Discussion..........................................................................................................32

3.1 Temporal Development of Horizontal Vortices...................................................32

3.2 Instantaneous Flow Field.....................................................................................44

3.3 Temporally-averaged Flow Field.........................................................................46

Figure 3. 1 Variation of water surface elevation at measurement point (numerical calculation)................................................................................................33

Figure 3. 2 Variation of wave length at measurement point (numerical calculation).......................................................................................................................33

Figure 3. 3 Result of FFT.............................................................................................34

Figure 3. 4 Temporal development of horizontal vortices; Spatial distribution velocity at (a) t=10 sec, (b) t = 30 s.............................................35

Figure 3. 5 Temporal development of horizontal vortices; Spatial distribution vorticity at (a) t=10 sec, (b) t = 30 s............................................38

Figure 3. 6 Temporal development of horizontal vortices; spatial distribution water surface at (a) t=10 sec, (b) t = 30 s.............................41

Figure 3. 7 2D velocity with water surface contour........................................45

Figure 3. 8 2D velocity with vorticity contour...................................................45

Figure 3. 9 Temporal variation of free surface (measured).........................46

Figure 3. 10 Calculated variation of free surface.........................................46

Figure 3. 11 Transverse profiles of mean velocity.......................................47

Table 3. 1 Comparison value of wavelength ( )................................................................32

48