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Saturday Pond Water Testing Programs

Water Quality Test Results 2000 - 2009

2009

August 27, 2009: Lew Wetzel conducted the Phosphorous test:

Phosphorous: 7 parts per billion in the deepest part (basin).

 

Secchi Disk readings from Carl Anderson - 2009
All depths are in meters
Date Depth Date Depth
21-May 6.59 4-Aug 5.24
3-Jun 6.11 4-Aug 5.40
3-Jun 5.33 19-Aug 5.59
17-Jun 6.51 19-Aug 5.44
17-Jun 6.49 1-Sep 6.71
9-Jul 5.64 1-Sep 6.80
9-Jul 5.69 16-Sep 7.10
15-Jul 6.27 29-Sep 7.05

 

2008

Secchi Disk Readings
Date Depth (m) Location Tester Conditions
06/17/08 5.05 Eric Groves 1:50 PM, 01 MPH wind, SW direction, cloudy, bright. heavy layer of pollen on surface. esp near shore
08/18/08 5.85 Eric Groves 10:45 AM; 04 MPH wind, SE direction, bright sky, did not hit bottom
07/17/08 6.05 Carl Anderson Large wake boat disturbing water most of day
08/20/08 6.51 Carl Anderson Strong wind all day
09/15/08 5.41 Carl Anderson Very strong wind with many white caps on day before
10/15/08 7.11 Carl Anderson Disc on bottom

2007

Secchi Disk Readings
Date Depth (m) Location Tester Conditions
07/22/07 6.25, 6.30 Ruth Wilson
07/23/07 6.04 Carl Anderson
08/01/07 6.96 deepest point Eric Groves 9:45 AM, sunny, no wind
08/18/07 6.70 deepest point Ruth Wilson 10:30 AM, wind 8 MPH
08/20/07 7.11 deepest point Eric Groves 2:23 PM, cloudy, bright, did not hit bottom
09/02/07 6.52 deepest point Eric Groves 11:35 AM, bright, wind 3 MPH NW, did not hit bottom
09/18/07 6.82 deepest point Carl Anderson
10/03/07 7.10 deepest point Carl Anderson

August 18, 2007: Lew Wetzel, assisted by Ruth Wilson and Eric Williams, conducted the following tests:

Phosphorous: 7 parts per billion in the deepest part (basin).

Bottom: 23.9'

Conditions: Air Temp = 62 F, Time = 1020 hrs, Wind = 08, direction = N

Temperature and Dissolved Oxygen Profiles-deepest part (basin)
Depth (m) degC Dissolved O2 (ppm)
0.0 22.9 8.3
1.0 23.0 8.2
2.0 23.1 8.3
3.0 23.1 8.3
4.0 23.1 8.3
5.0 23.1 8.3
6.0 23.0 8.3

2006

Aug 30, 2006: Lew Wetzel took a sample and had it analyzed at the U Maine Orono lab:
Phosphorous: 5 parts per billion.

Secchi Disk Readings
Date Depth (m) Tester
05/29/06 5.65, 5.60 Ruth Wilson
06/17/06 6.89, 6.95 Ruth Wilson
06/25/06 6.65, 6.70 Ruth Wilson

2005

August 14, 2005: Lew Wetzel conducted the following tests:

Phosphorous: 6 parts per billion in the northwest cove; 6 parts per billion in the deepest part (basin).

Secchi reading at deepest part: 6.40 meters

Conditions: Air Temp = 75 F, Time = 1040 hrs, Wind = 02, direction = NE

Temperature and Dissolved Oxygen Profiles-deepest part (basin)
Depth (m) degC Dissolved O2 (ppm)
0.0 26.4 8.0
1.0 26.4 7.9
2.0 26.3 7.9
3.0 26.0 7.8
4.0 25.5 7.5
5.0 20.6 5.7
6.0 15.7 2.6
7.0 14.1 1.5

2004

September 2004: Lew Wetzel conducted phosphorous testing on the pond during September 2004. The results were improved from previous readings.

Phosphorous: 5 parts per billion in the northwest cove; 6 parts per billion in the deepest part (basin).

Previous Phosphorous tests - See 1984-90 and 1995

July 27, 2004: Scott Lennox reported on his water test results. He and his daughter Mandy took measurements on July 27, 2004 at 8:30 AM. The sky was overcast, wind was 0 MPH, outside temperature was 17.5 C and the water depth at the sample point was 7.25 meters.

Secchi Disk reading: 6.05 meters.

Temperature and Dissolved Oxygen Profiles
Depth (m) degC Dissolved O2 (ppm)
6.5 16.0 2.4
5.5 19.5 5.2
4.0 22.5 8.4
1.0 22.5 11.2

2000

Report from Scott Lennox:

Periodic testing of the lake occurred from June to October with results consistent with the findings from previous years. Where our observations differed from 1998, they tended to be slightly improved.

The annual summer temperature stratification began to develop in June and was fully developed by July. Our July 30 testing provided a surface temperature of 26 degrees C (80 degrees F) and a 6.5 meter (21 feet) temperature of 20 degrees C (68 degrees F). This effect had disappeared with our last measurements in October. Our July water samples indicated correspondingly reduced levels of dissolved oxygen at each deeper level again consistent with or slightly better than 1998 levels. Our final monitoring revealed that the summer stratification had completely disappeared and we obtained a uniform temperature and level of dissolved oxygen.

Our Secchi disk monitoring of water clarity provided results that varied from typical 5.9 meters (19.5 feet) in July to an impressive 7.45 meters (24.5 feet) in October. This is significant because we conduct our testing in the deepest part of the lake (25 feet), and, as such, this measurement is likely to represent the top end of our potential results. One partial explanation for the improved results lies in the use of our new improved viewing scope, provided to us by the Maine DEP during our re-certification program. Secchi disk testing must be done with both scopes and reported to the Maine DEP separately. The use of the new scope can improve results up to 0.3 meters.

As with last year, these results compare favorably to the findings of prior years as far back as the mid 1980s. While the weather was above normal in warmth and brightness during the summer, the spring and fall also experienced significant storms and resulting runoff. Despite this, the test results, particularly in September and October, were among our best ever.