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“Human Impacts on Sediment in
         Faga’alu“




     by Alex Messina, MS Watershed Science
Thank you to our collaborators in
       American Samoa:

             CRAG
             DMWR
              DOC
             ASEPA

         ASCC/DOC-Intern:
          Rocco Tinitali
Motivation and Research Question

Land-based sources of sediment and nutrients
can damage coral…




Pristine Southern reef       Damaged Northern reef

 …so where and when is the sediment generated in
 the watershed?
What is a watershed and why is it
 important for Faga’alu Reefs?

 *Source and transportation
  of sediment and pollutants
  that can harm coral
 ecosystems


Storms cause muddy plume
from stream to reefs
Turbid,
                               freshwater layer
                               during rains



                                  Polluted,
                                  degraded
                                  ecosystem
Shallow, near rivermouth

                           Deeper, near reef crest




  Pristine,
  functioning
  ecosystem
A history of monitoring in Faga’alu
 •E. Bardi, 2005: Showed that Faga’alu was
  highly impacted by turbidity relative to other streams

 •P. Houk, 2006: Related coral health to stream water
  quality and showed Faga’alu as highly degraded

 •M. Sabater, 2007: Measured high rates of
  sediment accumulation on reefs in Faga’alu

 •S. Curtis, 2011: Measured stream water quality
  parameters up and down stream to identify likely
  sources of sediment runoff
Objectives:

 1) Reconnaissance of watershed to identify likely
     sources of sediment and nutrients

 2) When, How much: Quantify streamflow,
    sediment, and nutrients during storm
    and inter-storm periods

 3) Where: Where does the sediment go?

 4) Watershed model and management scenarios

 5) Build capacity for field monitoring and land-
     based pollution assessment in A.S.
Two parts:
•Upper natural/undisturbed portion
•Lower developed/impacted portion


                                     Tutuila, Am.Samoa
Potential Sediment Source: Natural Areas
Landslides, pig disturbance?




                       m
                       0
                     15




 Can be a natural, significant source of sediment
 but recover quickly
Potential sources: Quarry, urban areas, agriculture

                       1 km




  150 m




                       Sept, 2009
Quarry:

High levels of
sediment runoff
during rains




Key factor seems to
be rainfall intensity
Quarry:

                      Flat, high traffic areas
                      produce very turbid runoff




Inadequate sediment
control practices
…for now…
Some quarrying activities/groundwater flow maintain
high turbidity even under dry conditions
Possible source:
 Hospital storm drain
Conclusion from reconnaissance:

 Sediment is most important,
     sources include:
    1. Quarry
    2.   Hospital storm drain/urban area
    3.   Unpaved areas/sparse grass
    4.   Agriculture
    5.   Landslides
Objectives:

 1) Reconnaissance of watershed to identify likely
     sources of sediment and nutrients

 2) When, How much: Quantify streamflow,
    sediment and nutrient loading during storm
    and inter-storm periods

 3) Where: Where does the sediment go?

 4) Watershed model and management scenarios

 5) Build capacity for field monitoring and land-
     based pollution assessment in A.S.
4 Tipping Bucket rain gauges


1 Rain gauge on Mt. Matafao:
   • 2,142 feet, Highest point on the island
   • Very difficult access trail, ~35% slope
   • Starting point of watershed
Objective 2: Load (tons) = Q x C
 Measure stream flow (Q) and sediment concentration (C) at 3 locations
    a) Upper watershed (“Dam”, PT#3)
    b) Stream below quarry (“Quarry”, PT#2)
    c) Outlet to the ocean (“LBJ”, PT#1)
North
North




                      0.5mi.
Measuring stream flow (Q)   (L/sec)


                                             Measure depth
                                             Or “Stage”
                                             (like a ruler)



                              Outlet site


                                            Flow measurements
                                            relate “Stage” to
    Stage




                                            streamflow (Q)
                                            (Height to Volume)




                                              Measuring flow at
                                              dam above quarry
Measuring sediment (C): Storm, inter-storm sampling
     a. Manual/Auto sampling - six storms, >300 samples
     b. Turbidimeter – continuous, January – May 2012, two sites
            Convert turbidity to sediment concentration using
                            observed relationship




                              Auto-sampler at Quarry site




                                Filtering and weighing sediment
                                at DMWR lab
Increased sediment during stormflows




1/27/12
3:15pm    3:30pm    3:45pm     4:30 pm      6:00pm
Results: Example from one sampled storm
                    (March 7, 5.6 cm of rain)

       •Sediment load highest at LBJ, outlet to ocean
       •Responsive to rainfall – essential to monitor storms




•Sediment flux higher near hospital
•Responsive to rainfall
                                        Turbidimeter above quarry
Results: Storm Data                                                  % of Total
                                              Sediment(Tons)         Sediment
                Duration Precipitation
  #    Date      (Days)     (mm)       Upper    Lower     Total     Upper Lower
  1   1/31/12     11         224       0.88      7.28     8.15       10     89
  2   2/05/12     2.5        104       0.73      4.84     5.57       13     86
  3   3/05/12     2.5         78       0.31      1.12     1.43       21     78
  4   3/08/12      3          50       0.43      0.26     0.69       62     37
  5   3/15/12      4          88       0.15      0.53     0.68       22     77
  6   3/16/12      3          77       0.16      0.49     0.65       23     76
      Total:      26         621        3         15     Average:    26     74


  74% of sediment comes from the human- impacted
  lower watershed, most of it from the quarry

  26% of sediment comes from the upper
   watershed from natural erosion and landsliding

  Over 90% of sediment is moved during storms
Objectives:

 1) Reconnaissance of watershed to identify likely
     sources of sediment and nutrients

  2) When, How much: Quantify streamflow
sediment and nutrient loading during storm and
inter-storm periods

 3) Where: Where does the sediment go?

 4) Watershed model and management scenarios

 5) Build capacity for field monitoring and land-
     based pollution assessment in A.S.
Measuring sedimentation rates
 on Faga’alu reef (pilot study)
    1. Differences between North and South reefs
    2. Gradient away from rivermouth
    3. Only 2 Monthly samples: Feb and March

Hypothesized flow, and sediment accumulation
                                                   Assembly



               N
                   e r
                 rg ve




                                 ater
               ha ri
             sc id




                                 h
                            Seaw
           di rb




                            Fres
             Tu




                    S



                                                   Installation
Improving models with new datasets
   MODELS: Predict sediment load based on processes but need
                       to be calibrated to local conditions

   Model Objectives:
                        1. Scientific
                               a. Extend existing datasets
                               b. Quantify human impacts
                        2. Management
                               a. Scenarios
                               b. Watersed prioritization
Equations developed for                Map-based tools developed in
mid-west agricultural management       the tropics for coral conservation
Objectives:

 1) Reconnaissance of watershed to identify likely
     sources of sediment and nutrients

  2) When, How much: Quantify streamflow
sediment and nutrient loading during storm and
inter-storm periods

 3) Where: Where does the sediment go?

 4) Watershed model and management scenarios

 5) Build capacity for field monitoring and land-
     based pollution assessment in A.S.
Human Impacts on Sediment in Faga'alu
Next phase: CRTF Priority Watershed
                ->Management and Restoration
• If BMPs implemented at the quarry, and Village Watershed Plan
        implemented, how much is sediment reduced?
• How much coral will grow back naturally? With help?


                        •Sediment control at quarry

                        •Village Watershed Protection
                           Plan implemented

                        -->cleaner stream




                         •Less sediment on reef

                         •Coral restoration

                          --> healthier coral
Fa’afetai!

Questions?

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Human Impacts on Sediment in Faga'alu

  • 1. “Human Impacts on Sediment in Faga’alu“ by Alex Messina, MS Watershed Science
  • 2. Thank you to our collaborators in American Samoa: CRAG DMWR DOC ASEPA ASCC/DOC-Intern: Rocco Tinitali
  • 3. Motivation and Research Question Land-based sources of sediment and nutrients can damage coral… Pristine Southern reef Damaged Northern reef …so where and when is the sediment generated in the watershed?
  • 4. What is a watershed and why is it important for Faga’alu Reefs? *Source and transportation of sediment and pollutants that can harm coral ecosystems Storms cause muddy plume from stream to reefs
  • 5. Turbid, freshwater layer during rains Polluted, degraded ecosystem Shallow, near rivermouth Deeper, near reef crest Pristine, functioning ecosystem
  • 6. A history of monitoring in Faga’alu •E. Bardi, 2005: Showed that Faga’alu was highly impacted by turbidity relative to other streams •P. Houk, 2006: Related coral health to stream water quality and showed Faga’alu as highly degraded •M. Sabater, 2007: Measured high rates of sediment accumulation on reefs in Faga’alu •S. Curtis, 2011: Measured stream water quality parameters up and down stream to identify likely sources of sediment runoff
  • 7. Objectives: 1) Reconnaissance of watershed to identify likely sources of sediment and nutrients 2) When, How much: Quantify streamflow, sediment, and nutrients during storm and inter-storm periods 3) Where: Where does the sediment go? 4) Watershed model and management scenarios 5) Build capacity for field monitoring and land- based pollution assessment in A.S.
  • 8. Two parts: •Upper natural/undisturbed portion •Lower developed/impacted portion Tutuila, Am.Samoa
  • 9. Potential Sediment Source: Natural Areas Landslides, pig disturbance? m 0 15 Can be a natural, significant source of sediment but recover quickly
  • 10. Potential sources: Quarry, urban areas, agriculture 1 km 150 m Sept, 2009
  • 11. Quarry: High levels of sediment runoff during rains Key factor seems to be rainfall intensity
  • 12. Quarry: Flat, high traffic areas produce very turbid runoff Inadequate sediment control practices …for now…
  • 13. Some quarrying activities/groundwater flow maintain high turbidity even under dry conditions
  • 15. Conclusion from reconnaissance: Sediment is most important, sources include: 1. Quarry 2. Hospital storm drain/urban area 3. Unpaved areas/sparse grass 4. Agriculture 5. Landslides
  • 16. Objectives: 1) Reconnaissance of watershed to identify likely sources of sediment and nutrients 2) When, How much: Quantify streamflow, sediment and nutrient loading during storm and inter-storm periods 3) Where: Where does the sediment go? 4) Watershed model and management scenarios 5) Build capacity for field monitoring and land- based pollution assessment in A.S.
  • 17. 4 Tipping Bucket rain gauges 1 Rain gauge on Mt. Matafao: • 2,142 feet, Highest point on the island • Very difficult access trail, ~35% slope • Starting point of watershed
  • 18. Objective 2: Load (tons) = Q x C Measure stream flow (Q) and sediment concentration (C) at 3 locations a) Upper watershed (“Dam”, PT#3) b) Stream below quarry (“Quarry”, PT#2) c) Outlet to the ocean (“LBJ”, PT#1) North North 0.5mi.
  • 19. Measuring stream flow (Q) (L/sec) Measure depth Or “Stage” (like a ruler) Outlet site Flow measurements relate “Stage” to Stage streamflow (Q) (Height to Volume) Measuring flow at dam above quarry
  • 20. Measuring sediment (C): Storm, inter-storm sampling a. Manual/Auto sampling - six storms, >300 samples b. Turbidimeter – continuous, January – May 2012, two sites Convert turbidity to sediment concentration using observed relationship Auto-sampler at Quarry site Filtering and weighing sediment at DMWR lab
  • 21. Increased sediment during stormflows 1/27/12 3:15pm 3:30pm 3:45pm 4:30 pm 6:00pm
  • 22. Results: Example from one sampled storm (March 7, 5.6 cm of rain) •Sediment load highest at LBJ, outlet to ocean •Responsive to rainfall – essential to monitor storms •Sediment flux higher near hospital •Responsive to rainfall Turbidimeter above quarry
  • 23. Results: Storm Data % of Total Sediment(Tons) Sediment Duration Precipitation # Date (Days) (mm) Upper Lower Total Upper Lower 1 1/31/12 11 224 0.88 7.28 8.15 10 89 2 2/05/12 2.5 104 0.73 4.84 5.57 13 86 3 3/05/12 2.5 78 0.31 1.12 1.43 21 78 4 3/08/12 3 50 0.43 0.26 0.69 62 37 5 3/15/12 4 88 0.15 0.53 0.68 22 77 6 3/16/12 3 77 0.16 0.49 0.65 23 76 Total: 26 621 3 15 Average: 26 74 74% of sediment comes from the human- impacted lower watershed, most of it from the quarry 26% of sediment comes from the upper watershed from natural erosion and landsliding Over 90% of sediment is moved during storms
  • 24. Objectives: 1) Reconnaissance of watershed to identify likely sources of sediment and nutrients 2) When, How much: Quantify streamflow sediment and nutrient loading during storm and inter-storm periods 3) Where: Where does the sediment go? 4) Watershed model and management scenarios 5) Build capacity for field monitoring and land- based pollution assessment in A.S.
  • 25. Measuring sedimentation rates on Faga’alu reef (pilot study) 1. Differences between North and South reefs 2. Gradient away from rivermouth 3. Only 2 Monthly samples: Feb and March Hypothesized flow, and sediment accumulation Assembly N e r rg ve ater ha ri sc id h Seaw di rb Fres Tu S Installation
  • 26. Improving models with new datasets MODELS: Predict sediment load based on processes but need to be calibrated to local conditions Model Objectives: 1. Scientific a. Extend existing datasets b. Quantify human impacts 2. Management a. Scenarios b. Watersed prioritization Equations developed for Map-based tools developed in mid-west agricultural management the tropics for coral conservation
  • 27. Objectives: 1) Reconnaissance of watershed to identify likely sources of sediment and nutrients 2) When, How much: Quantify streamflow sediment and nutrient loading during storm and inter-storm periods 3) Where: Where does the sediment go? 4) Watershed model and management scenarios 5) Build capacity for field monitoring and land- based pollution assessment in A.S.
  • 29. Next phase: CRTF Priority Watershed ->Management and Restoration • If BMPs implemented at the quarry, and Village Watershed Plan implemented, how much is sediment reduced? • How much coral will grow back naturally? With help? •Sediment control at quarry •Village Watershed Protection Plan implemented -->cleaner stream •Less sediment on reef •Coral restoration --> healthier coral