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Water Quality Investigation of Agua Caliente Spring Martha Conklin & Roger Bales University of Arizona Background on Agua Caliente Science questions &

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Presentation on theme: "Water Quality Investigation of Agua Caliente Spring Martha Conklin & Roger Bales University of Arizona Background on Agua Caliente Science questions &"— Presentation transcript:

1 Water Quality Investigation of Agua Caliente Spring Martha Conklin & Roger Bales University of Arizona Background on Agua Caliente Science questions & hypotheses Results of initial investigations

2 Agua Caliente, a county park, starts as a small spring, an oasis in the semi-arid Sonoran Desert

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5 Observations Perennial spring Flow rate varies throughout the year Water temperature at source is not very sensitive to air temperature

6 Research Questions Why does it flow all year? Where does the water come from? Why is it warm at its source?

7 Data Sources A GLOBE school, Fort Lowell Elementary in Tucson, AZ, has been making measurements at 2 sites at Aqua Caliente Water agency data are available from several groundwater wells within a few km of the site

8 Agua Caliente Temperatures 5 10 15 20 25 30 35 5101520253035 Air Temp. ºC Water Temp. ºC Pond 1 entrance Pond 1 island GLOBE data, Ft. Lowell Elementary

9 Hypothesis Accepted explanation: The water comes from a higher elevation. It follows a deep flow path and a fracture in the bedrock allows it to surface. Our hypothesis: The water source must be a mixture of deep ground water and shallow recharge.

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11 Approach Locate existing data sources Develop a sampling plan to test our hypothesis, i.e. determine if the water composition and temperature vary with flow rate.

12 Chemical Comparison Parameter Deep well a Aqua Caliente b Shallow well a Electrical conductivity1200750500 Alkalinity, mg/L146184174 pH8.18.29.6 R. Kalin Ph.D dissertation, 1998 GLOBE data, Ft. Lowell Elementary a b

13 Detailed Chemical Analyses Constituent, mg/L Deep well a Aqua Caliente b Shallow well a Ca 2+ 142537 Mg 2+ 325 Na + 15513340 SO 4 2- 31716241 Cl - 342710 NO 3 - - 2 - R. Kalin Ph.D dissertation, 1998 Recent analyses, UA HWR a b

14 Conclusions The composition does not match other deep ground water; it appears to be a mix of shallow and deep ground water. Seasonal changes are important; time series data are needed to understand seasonal cycles

15 Proposed Weekly Measurements Conductivity, pH and alkalinity (GLOBE) Flow rate of spring Water chemistry: Ca 2+, Mg 2+, Na +, Cl -, SO 4 2-, NO 3 -

16 Footnote on GLOBE Data Very useful for starting the investigation Good supplemental source for continuing longer-term investigations


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