Bacterial Quality of Crystalline Rock and Glacial Aquifers in New England

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Bacterial Quality of Crystalline Rock and Glacial Aquifers in New England By Sarah Flanagan and Charles Culbertson, U.S. Geological Survey 2012 New Hampshire Water and Watershed Conference Plymouth State University, Plymouth, N.H. March 23, 2012

Acknowledgments Kelly Warner, Wayne Lapham, and Michael Yurewicz, USGS NAWQA Program Kellie McMahon, NH/VT Water Science Center McKenzie Parker, Maine Water Science Center Amie M.G. Brady, USGS Ohio Microbiology Lab Brandon Kernen, NH Department of Environmental Services

Objectives Describe methods of collecting total coliform and Escherichia coli bacteria, and coliphage virus samples for the U.S. Geological Survey s National Water-Quality Assessment (NAWQA) Groundwater Trends Program Assess factors relating to occurrence of bacteria in wells Select findings

Method of Analysis EPA Method 1604: Total Coliform and Escherichia coli bacteria by membrane filtration using simultaneous detection and enumeration (MI agar medium). Replicate samples collected and processed in the field within 1 hour of collection for each well. EPA Method 1601: A performance-based method for detecting the presence of male-specific (F+) and somatic coliphage in water. Samples are analyzed within 48 hours by the USGS Microbiology Lab in Columbus, OH. A male-specific phage infects male host strains of E. coli. A somatic phage infects E. coli via their cell membrane.

Plated Live TC and E. Coli Bacteria [under ambient light]

Total Coliform illuminated under black light

Location of wells sampled for the Location USGS of National wells Water-Quality Assessment (NAWQA) Program, (2002-2011) n=105

Time line of NAWQA Bacteriological Sampling in New England

Comparison of Bacteria and Coliphage Detections in Drinking-water Wells in New England with the Nation WATER USE - AQUIFER # SAMPLES TOTAL COLIFORM ESCHERICHIA COLI F+ COLIPHAGE SOMATIC COLIPHAGE DOMESTIC BEDROCK 26 19 (73 %) 0 0 2 (8 %) PS BEDROCK 14 0 0 0 0 DOMESTIC GLACIAL 18 2 (11 %) 0 0 0 PS GLACIAL 47 5 (11 %) 0 0 0 ALL NAWQA wells used for drinking-water 715/191 (27 %) 741/54 (7 %) 420/14 (3.2 %)

Distribution of Total Coliform, By Well Network

Domestic Well Photos [ Do maintenance and construction practices factor in bacteria contamination?] Broken Cap Well hidden in a rock wall Well low to the ground

A small community water system in southeastern NH

Where Was Somatic Coliphage Detected?

The two domestic wells with detectable coliphage

Total Coliform Occurrence and Well Construction Properties

Total Coliform and Precipitation

Relation between Total Coliform and other Data

Relation between Total Coliform and other Data, cont

Significant Spearman s Rho Coefficients for Total Coliform [DOMESTIC BEDROCK wells] Correlation Variable N Coeff P-value Correlation Variable N Coeff P-value atrazine 26 0.43 0.03 CIAT 26 0.35 0.076 Ammonia 26-0.32 0.115 Na 26-0.30 0.136 Water Temp 26 0.30 0.143 PO 4 26-0.20 0.328 Well depth 26-0.19 0.349 Cl 26-0.186 0.361 DO % sat 26-0.178 0.385 Cu 26 0.174 0.39 NO 3 26 0.174 0.395 Br 26-0.15 0.476 ph 26-0.146 0.476 Water Level 25-0.137 0.512

Domestic Bedrock Wells, TC counts, and their lithology Total Coliform, colonies per 100 ml 370, 220, 130, 120, 11, 1, <1, <1 Bedrock Unit Vassalboro Formation Lithology Calcpelite >100, >100, 30, 7, 6, <1 Sangerville Formation Calcgranofels, Carbonate Rocks 44, 2 Kittery Formation Calcgranofels 4 Elliot Formation Calcgranofels 2, 2 Madrid Formation Calcpelite 2 Rindgemere Formation Pelitic Rocks 2, <1, <1 Berwick Formation Calcgranofels <1, <1 Waterville Formation Pelitic Rocks Public Supply Bedrock Wells <1, <1, <1, <1 Berwick Formation Calcgranofels <1, <1, <1, <1 Kittery Formation Calcgranofels <1, <1, Exeter Diorite Mafic Rocks <1, <1, <1 Rye Complex Two-mica granite <1 Elliot Formation Calcgranofels

Another example of a PS well located in a protected zone

Older Gravel-Packed Glacial PS Well located in an urban setting

Comparison Between USGS and NHDES Results WELL Location USGS source 100 ml NHDES source 100 ml USGS Kitchen 100 ml NHDES Kitchen 100 ml Method EPA 1604 SM 9222B EPA 1604 SM 9222B Lee, NH 0 0 0 0 Kensington, NH 5 6 1,750 >200 Salem, NH 1 0 -- -- *EPA 1604 Method = MI Agar media and membrane filtration. *SM9222B Method = M-Endo agar media and membrane filtration. NOTE: Both methods produced NEG results for e. coli.

Select Findings of the study Of 26 domestic bedrock wells, 19 had detectable Total Coliform (TC), 2 had detectable somatic coliphage, but none had detectable E. coli. In one domestic bedrock well, the sample from the pressure tank (the source) had 5 TC colonies and the sample from the kitchen sink had more than 1,700 TC colonies. Of the 2 domestic bedrock wells with detectable somatic coliphage, one well had TC present (30 colonies per 100 ml), but the second well was absent of TC. Neither well had detectable E. coli. Of 14 public-supply bedrock wells, no detections for TC, E. coli, and coliphage. Domestic wells completed in the Vassalboro and Sangerville bedrock units had greater occurrence of TC and higher TC counts than other bedrock units.

Risk factors for bacteria detections in wells may include: Wells used for domestic supply. Wells completed in fractured bedrock. High Darcian flow rates. Vertical fracture orientation. Little ability to filter water. Heavy rainfall events or when groundwater is recharged. Good hydrologic connection to land surface or nearby surface water. Condition of well.