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Cypress Creek / Blanco River Data Summary Report
Cypress Creek / Blanco River Data Summary Report
Cypress Creek / Blanco River Data Summary Report
Cypress Creek / Blanco River Data Summary Report
Cypress Creek / Blanco River Data Summary Report
Cypress Creek / Blanco River Data Summary Report
Cypress Creek / Blanco River Data Summary Report
Cypress Creek / Blanco River Data Summary Report
Cypress Creek / Blanco River Data Summary Report
Cypress Creek / Blanco River Data Summary Report
Cypress Creek / Blanco River Data Summary Report
Cypress Creek / Blanco River Data Summary Report
Cypress Creek / Blanco River Data Summary Report
Cypress Creek / Blanco River Data Summary Report
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Cypress Creek / Blanco River Data Summary Report

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Cypress Creek / Blanco River Data Summary - March 2012

Cypress Creek / Blanco River Data Summary - March 2012

Published in: News & Politics, Technology
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  • Shaded area is sites on Blanco River
  • This points to buildup on surface (or in channel sediments) during low flow, then wash out when rains start again.
  • This pattern points to local source of ammonia in creek during low flows, perhaps animal feces directly in creek or leaky septic systems?
  • Transcript

    • 1. Cypress Creek & Blanco River Data Summary David BakerWimberley Valley Watershed Association March 22, 2012
    • 2. • Groundwater & surface water interactions are critical to water quality in Cypress Creek
    • 3. Geologic SettingSource: HTGCD, 2010
    • 4. Summary of CRP Data• Differences in data from the Cypress Creek to the Blanco River reflect their different sizes, flow patterns, and catchment areas.• Water quality at Jacob’s Well and Blue Hole strongly influenced by groundwater interactions• Other sites show broader range of values and greater influence from surface conditions (runoff, weather, NPS pollution)• Droughts of 2008-2009 and 2010-2011 had significant impact on water quality in the Wimberley Valley
    • 5. Upstream toDownstream Trends
    • 6. E. coli• Average bacteria level rises as you travel downstream in the Cypress Creek: – 51 cfu/100mL at Jacob’s Well – 262 cfu/100mL at the Blanco confluence• All sites have E. coli grab samples above the standard• Maximum readings: – 3830 cfu/100mL in the Cypress Creek-Blanco confluence (Aug 2011) – 4800 cfu/100m in the Blanco River downstream from Wimberley (Mar 2006)
    • 7. Dissolved Oxygen• DO rises on average as you travel downstream in Cypress Creek• Relatively constant at Jacob’s Well (average = 6.0 mg/L, standard dev = 1.2 mg/L)• For Cypress Creek, summer of 2011 caused record low DO readings at 4 downstream sites• At Jacob’s Well and on Blanco River, lowest recorded DO was in Aug 2007
    • 8. Dissolved Oxygen and Flow• Dissolved oxygen at Jacob’s Well not as sensitive to flow• Relatively constant (average 6.0 mg/L) DO from groundwater input
    • 9. Dissolved Oxygen and Flow• Other sites show strong influence of flow on DO, both Cypress Creek and Blanco River
    • 10. NPS pollution - Nitrogen• Rising flow following extended dry periods in 2009 and 2011 caused very high peaks in nitrogen at all sites in Cypress Creek.• Blanco River sites show the same pattern, too.
    • 11. NPS pollution - Ammonia• On the contrary, higher than normal ammonia observed during extended dry period in 2011• Record high ammonia recorded at Jacob’s Well in Feb 2012
    • 12. Summary• Dissolved oxygen remains a critical issue when flow is reduced; record low levels observed in summer 2011• E. coli levels occasionally very high, but in general observations have been lower in 2009-11 than in 2005- 08• Data show that nitrogen is built up during extended dry periods and spikes after rainfall• Ammonia peaks during extended dry periods, suggesting a source close to the river (wildlife or septic systems)• At all sites (Blanco and Cypress), ammonia readings have been much higher in 2009-11 (avg 0.09 mg/L) versus 2005-08 (0.03 mg/L)

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