Assessment of Runoff, Sediment Yield and Nutrient Load on Watershed Using Watershed Modeling
description
Transcript of Assessment of Runoff, Sediment Yield and Nutrient Load on Watershed Using Watershed Modeling
Assessment of Runoff, Sediment Yield and Assessment of Runoff, Sediment Yield and Nutrient Load on Watershed Using Nutrient Load on Watershed Using
Watershed ModelingWatershed Modeling
Mohammad Sholichin Mohammad Sholichin 1)
Faridah Othman Faridah Othman 2)2)
Shatirah Akib Shatirah Akib 3)3)
1) Lecturer, Water Resources Department, Brawijaya University, Indonesia
PhD Student, Department of Civil Engineering, Universiti Malaya, Malaysia;
2) Lecturer, Department of Civil Engineering, Universiti Malaya, Malaysia
3) PhD Student, Department of Civil Engineering, Universiti Malaya, Malaysia
BackgroundBackground• Increasing population people, wastewater from Increasing population people, wastewater from
industry and fertilizer use for farmer become industry and fertilizer use for farmer become water quality problem in stream. water quality problem in stream.
• Main problem in Upstream Brantas River Basin Main problem in Upstream Brantas River Basin are land erosion, sedimentation and pollutant are land erosion, sedimentation and pollutant load from both agricultural area and load from both agricultural area and residentialresidential
• Propose of watershed modeling (AVSWAT) to Propose of watershed modeling (AVSWAT) to predict water quality by difference predict water quality by difference management practice management practice
The main objective of this research are :The main objective of this research are :• to assessment of runoff, sediment yield to assessment of runoff, sediment yield
and nutrient load at Watershedand nutrient load at Watershed• To identification of potentially source of To identification of potentially source of
sediment and nutrient load on watershed sediment and nutrient load on watershed • to propose the relationship relating to propose the relationship relating
sediment and nutrient loads to sediment and nutrient loads to physiographic and hydrologic properties physiographic and hydrologic properties of the each sub watershed of the each sub watershed
The Case StudyThe Case Study
Upstream Brantas RiverUpstream Brantas RiverUpstream Brantas
Banggo River Basin
Amprong River Basin
Upper Lesti River Basin
Genteng River Basin
Metro River Basin
Manten River Basin
Lower Lesti River Basin
Kedung BantengRiver Basin
Soil Water Assessment Tool Soil Water Assessment Tool (SWAT)(SWAT)
• Uses physically-based input such as soil, weather, Uses physically-based input such as soil, weather, land use, and topographic data to predict the impact land use, and topographic data to predict the impact of land management practice on water, sediment, of land management practice on water, sediment, and agricultural chemical yieldsand agricultural chemical yields
• Continuous Long-term Simulation on daily stepContinuous Long-term Simulation on daily step• Assesses impacts of climate and management on Assesses impacts of climate and management on
yields of water, sediment, and agricultural chemicalsyields of water, sediment, and agricultural chemicals
Processing and Display of AVSWAT Model
Schematic of input and outputs of the AVSWAT model
AVSWAT Routing PhaseAVSWAT Routing Phase• Flow routingFlow routing
- Inputs (runoff, rain, point-source discharge)- Inputs (runoff, rain, point-source discharge)- Outputs (evaporation, transmission, extraction for - Outputs (evaporation, transmission, extraction for
human use)human use)• Sediment routing: deposition, resuspension, Sediment routing: deposition, resuspension,
erosionerosion• Nutrient RoutingNutrient Routing
- Model dissolved and adsorbed nutrients.- Model dissolved and adsorbed nutrients.- In stream kinetics adapted from QUAL2E- In stream kinetics adapted from QUAL2E
1. Land Phase
Phosphorous Cycle
2. Routing Phase
• Period of Calibration: January 1, 1992 – Dec 2002• Period of Validation : Jan 1 2003 – Dec 31 2006• Rainfall/Runoff/Routing: Daily Rain/Curve
Number/Daily• Rainfall Distribution: Normal Skewed• Potential ET Method: Priestley-Taylor method• Channel Water Routing: Muskingum• Channel Degradation: Not Active• Stream Water Quality Processes: Active• Lake Water Quality Processes: Not Active• Printout Frequency: Monthly and Annually
SWAT Setup Preparation
Slope Classification
Slope Down AreaSlope Down Area
Land use Land use MapMap
Soil Type Map
Comparison Observed-Simulated
0
50
100
150
200
250
J
1992 1993 1994 1995 1996 1997 1998 1999 2000 2001 2002
year
Dis
char
ge (m
3/se
c)
Observed Simulated
Calibration PeriodCalibration Period
Correlation ValueCorrelation ValueLinier Correlation of Observed - Simulated
y = 1.05x - 9.31R2 = 0.85
0
50
100
150
200
0 50 100 150 200
Observed
Sim
ulat
ed
z
Results1. Land Area Phase
-500
1,0001,5002,0002,5003,0003,5004,000
Ban
ggo
Riv
er
Ups
tream
Bra
ntas
Am
pron
g R
iver
Ked
ung
Ban
teng
Met
ro R
iver
Man
ten
Riv
er
Low
er L
esti
Riv
er
Upp
er L
esti
Riv
er
Gen
teng
Riv
er
Basin Name
Rai
nfal
l (m
m) &
Run
off (
mm
)
050100150200250300350400
Bas
in a
rea
(km
2)
Rainfall (mm) Runoff (mm) Area (km2)
Sediment Yield (ton/ha/yr)Sediment Yield (ton/ha/yr)
- 20 40 60 80 100
Banggo River
Upstream Brantas
Amprong River
Kedung Banteng
Metro River
Manten River
Lower Lesti River
Upper Lesti River
Genteng River
Bas
in N
ame
Sediment Yields (ton/ha)
Sediment Yield (ton/ha/yr)Sediment Yield (ton/ha/yr)
> 1.741.74 – 4.534.53 – 7.887.88 – 27.3327.33 – 85.95
Upper Lesti River Basin
Amprong River Basin
Organic N (kg N/ha)Organic N (kg N/ha)
- 5 10 15 20 25 30 35
Banggo River
Upstream Brantas
Amprong River
Kedung Banteng
Metro River
Manten River
Lower Lesti River
Upper Lesti River
Genteng River
Bsi
n N
ame
Organic N (Kg N/ha)
Organic N (kg N/ha)Organic N (kg N/ha)Upstream Brantas
Bango River Basin
Organic P (kg P/ha)Organic P (kg P/ha)
- 1.0 2.0 3.0 4.0 5.0
Banggo River
Upstream Brantas
Amprong River
Kedung Banteng
Metro River
Manten River
Lower Lesti River
Upper Lesti River
Genteng River
Bas
in N
ame
Organic P (kg P/ha)
Organic P (kg P/ha)Organic P (kg P/ha)Bango River Basin
Annual Average Estimates of Sediment Annual Average Estimates of Sediment Yield and Nutrient Load for Each Basin Yield and Nutrient Load for Each Basin
Based on Period 1995 to 2006 Based on Period 1995 to 2006 SimulatedSimulated
2. In Stream
0.010.020.030.040.050.060.070.0
Ban
ggo
Riv
er
Ups
tream
Bra
ntas
Am
pron
g R
iver
Ked
ung
Ban
teng
Met
ro R
iver
Man
ten
Riv
er
Low
er L
esti
Riv
er
Upp
er L
esti
Riv
er
Gen
teng
Riv
er
Dis
char
ge (m
3/se
c)
-2004006008001,0001,2001,4001,6001,800
Sed
Con
cent
raui
n m
g/l)
Discharge (m3/sec) Sed concentration (mg/l)
Concentration of Organic N Concentration of Organic N & P& P
- 2 4 6 8 10
Banggo River
Upstream Brantas
Amprong River
Kedung Banteng
Metro River
Manten River
Lower Lesti River
Upper Lesti River
Genteng River
Concentration (mg/l)
Org POrg N
Annual Average Estimates of Nutrient Annual Average Estimates of Nutrient Concentration in outlet stream for Each Concentration in outlet stream for Each
Basin Based on Period 1995 to 2006 Basin Based on Period 1995 to 2006 SimulatedSimulated
Sediment concentration (mg/L)
0.0
1.0
2.0
3.0
4.0
5.0
6.0
1993
1994
1995
1996
1997
1998
1999
2000
2001
2002
2003
2004
2005
2006
3. In Reservoir
Concentration of N & P
0.00
0.10
0.20
0.30
0.40
0.50
0.6019
93
1994
1995
1996
1997
1998
1999
2000
2001
2002
2003
2004
2005
2006
Org NOrg P
ConclusionConclusion• Banggo river basin is both highest of rainfall Banggo river basin is both highest of rainfall
2.043 mm and surface runoff 876.67 mm, 2.043 mm and surface runoff 876.67 mm, respectivelyrespectively
• The highest sediment yield is 85,94 The highest sediment yield is 85,94 ton/ha/year in Upper Lesti river basin due to ton/ha/year in Upper Lesti river basin due to maximum erosion rate maximum erosion rate
• The concentration of organic P (range 0,36 – The concentration of organic P (range 0,36 – 0,99 mg/l) in all sub basin is over of the WQ 0,99 mg/l) in all sub basin is over of the WQ standard regulation in C class.standard regulation in C class.
• The concentration of organic N (range 9,34 – The concentration of organic N (range 9,34 – 20,80 mg/l) in all sub basins is lower of the 20,80 mg/l) in all sub basins is lower of the WQ standard regulation in C class.WQ standard regulation in C class.
• The AVSWAT model was successes for The AVSWAT model was successes for assessment of runoff, sediment yield and assessment of runoff, sediment yield and nutrient load in Upper Brantas River Basin nutrient load in Upper Brantas River Basin
SuggestioSuggestionn
• The AVSWAT model would be testing to The AVSWAT model would be testing to another watershed another watershed
• In the next simulation, modification of In the next simulation, modification of difference fertilizer used and management difference fertilizer used and management tillage in agriculture would be done. tillage in agriculture would be done.
• Simulation of SWAT model can also done Simulation of SWAT model can also done which difference of divided of each sub which difference of divided of each sub basin which smaller than 200 km2. basin which smaller than 200 km2.
AcknowledgemenAcknowledgementtWe would like to thank you the We would like to thank you the
following following for making this study possible:for making this study possible:
Brawijaya University, IndonesiaBrawijaya University, IndonesiaUniversity of Malaya, MalaysiaUniversity of Malaya, MalaysiaPerum Jasa Tirta I, Malang, IndonesiaPerum Jasa Tirta I, Malang, IndonesiaDepartment of Agriculture, IndonesiaDepartment of Agriculture, IndonesiaDepartment of Surveying, IndonesiaDepartment of Surveying, Indonesia
Thank Thank youyou