METHODS
Fifty-eight lakes were sampled from 1989 through 1993 while they were free of snow and ice (Table 2.2). Some lakes were sampled one to three times, whereas others were sampled up to 12 times during the 5-year study. The lakes were located in remote mountainous terrain, and were accessed by hiking or by helicopter. Sampling was conducted from an inflatable boat over the deepest spot in each lake. Water temperatures were determined at a depth of 1 m using an Omega HH70 hand-held thermometer. Water samples were collected 1 m below the surface of each lake using a 1.5-L Van Dorn-style bottle. Filtered (0.7-µm prewashed Watman GF/C filters) samples were placed in 1-L acid-washed, high-density polyethylene bottles for nutrient analyses. Unfiltered samples collected in 250 ml acid-washed polypropylene bottles were used for analyses of pH, alkalinity, and conductivity. To the degree possible, water samples were taken just before leaving the field to minimize sample deterioration. If samples were kept overnight in the field, the bottles were placed out of the light during the day or in dark bags and kept in the coldest spot that could be found (e.g., inlet stream, snow bank). When departing the field, the samples were wrapped with insulation to maintain coolness, transported out of the field, frozen, and then shipped to the Cooperative Chemical Analytical Laboratory, Oregon State University. Chemical analyses included pH, alkalinity, conductivity, total Kjeldahl-N, nitrate-N, ammonia-N, total phosphorus, and orthophosphate-P (Table 2.3).
Table 2.2. Elevations, surface areas, maximum depths, and vegetation zones and the number of times each lake was sampled (1989-93) for NOCA study lakes east and west of the hydrologic divide.
| Lake | Elevation (m) | Depth (m) | Surface Area (Ha) | Vegetation Zone1 | Times Sampled |
|---|---|---|---|---|---|
| East-Slope Lakes | |||||
| COON TRAPPER WADDELL BATTALION DOUBTFUL GREEN VIEW DAGGER MCALESTER RAINBOW M132 M131 MR11 MR2 MR3 LOWER TRIPLET MM11 UPPER TRIPLET JUANITA |
662 1270 1504 1629 1642 1664 1679 1679 1717 1789 1800 1863 1873 1873 1931 1974 1988 2033 |
8.2 59.0 4.1 2.5 12.0 16.1 3.6 5.0 6.3 1.2 0.3 1.3 0.3 0.2 1.0 1.4 1.0 0.2 |
5.8 49.0 11.9 4.3 17.7 47.3 4.0 6.1 10.4 5.0 2.0 8.8 1.5 1.5 2.1 7.6 4.3 1.2 |
4 2 3 3 2 2 3 3 3 2 2 2 2 2 2 2 2 2 |
2 2 7 4 4 2 3 7 8 8 6 7 6 4 4 2 4 3 |
| WEST-SLOPE LAKES | |||||
| THUNDER PYRAMID HOZOMEEN WILLOW RIDLEY LOWER PANTHER UPPER PANTHER NO NAME BOUCK PRICE LS1 LS2 MONOGRAM LOWER THORNTON LS3 MORAINE PM53 NERT MIDDLE THORNTON WILD JEANITA LOWER REVILLE EP6 MP8 VULCAN COPPER EGG SKYMO UPPER SKYMO KLAWATTI TALUS TARN OUZEL SWEET PEA TAPTO, MIDDLE TAPTO, WEST TAPTO, UPPER BEAR EILEY WILEY SILVER |
412 802 861 870 958 1031 1031 1171 1174 1188 1241 1243 1270 1357 1365 1378 1382 1388 1427 1488 1496 1525 1566 1566 1583 1601 1604 1609 1610 1624 1632 1659 1687 1754 1754 1755 1769 1982 2028 2063 |
3.0 0.3 38.4 8.2 4.3 0.2 0.1 4.4 5.2 16.0 0.4 2.0 12.7 23.5 1.5 32.5 1.0 1.0 5.0 4.6 0.5 1.6 3.0 0.9 3.3 5.2 0.8 4.3 3.0 12.0 0.6 2.0 3.4 0.3 0.8 4.0 11.4 1.0 2.4 65.1 |
6.4 8.8 19.0 3.7 9.8 5.8 3.0 9.1 19.0 26.2 3.4 4.7 37.2 33.0 4.9 33.0 9.1 8.2 24.0 8.8 2.4 3.0 19.8 3.7 6.4 22.6 4.9 5.5 4.3 33.0 3.6 9.8 27.4 5.5 4.3 13.1 46.3 4.6 -- 137.0 |
4 4 4 4 4 4 4 3 3 2 3 3 2 3 2 1 3 3 2 2 3 2 2 1 2 2 2 2 1 1 2 1 3 2 2 2 2 1 1 1 |
4 9 2 2 1 12 10 1 1 1 10 10 1 2 1 1 2 1 1 1 1 2 1 1 1 1 2 2 1 1 1 1 3 3 3 1 1 1 1 |
Alpine (1), subalpine (2), high-forest (3), and low forest (4)
Table 2.3. Analytical procedures used by the Cooperative Chemistry Analytical Laboratory, Oregon State University.
| Variable | Method | Detection limits |
(Units) |
|---|---|---|---|
| pH | Portable Beckman meter 21. Orion Surflow Standardized with pH 4 and pH 7 buffers. Final reading recorded after 5 consecutive readings of the same value (usually 30-45 minutes) | 0-14 | Standard |
| Alkalinity | Electrometric titration to pH 4.5 | 0.2 | (mg/l) |
| Conductivity | Wheatstone Bridge, Yellow Spring model 33, corrected to 25°C | 0.4 | (µS/cm) |
| Nitrate-N | Technicon Autoanalyzer, automated cadmium reduction | 0.001 | (mg/l) |
| Kjeldahl-N | Nessler's Reagant finish | 0.01 | (mg/l) |
| Ammonia-N | Technicon Autoanalyzer, colormetric automated phenate | 0.05 | (mg/l) |
| Total Phosphorus | Persulfate digestion, ascorbic acid finish | 0.001 | (mg/l) |
| Orthophosphate-P | Reactive phosphate, ascorbic acid finish | 0.001 | (mg/l) |
Dates of ice-out, defined as the time when the lake surfaces were virtually ice-free, were estimated for most lakes from aerial surveys conducted in 1989 when the field crews were helicoptered to and from sampling locations. The estimated dates of ice-out likely were within 1 to 2 weeks of the actual dates in some cases. For a few lakes not covered by the aerial surveys, estimated dates of ice-out were obtained from backcountry park rangers.
Average values for the water-quality variables were calculated using
the STATS module of SYSTAT (Wilkinson 1987). Average pH was calculated
from hydrogen ion activity. Regression analyses were used to evaluate
dates of ice-out and changes in water quality with increased lake
elevation for lakes west of the hydrologic divide using the MGLH module
of SYSTAT. West-slope NOCA lakes were used because samples were
available from a greater range of lake elevation (i.e., alpine to
low-forest lakes), than were east-slope lakes (primarily subalpine
lakes). Statistical comparisons of dates of ice-out and the water
qualities of east-slope and west-slope lakes in the subalpine vegetation
zone were conducted using the Mann-Whitney test (NPAR module of SYSTAT).
Level of statistical significance was
= 0.05.
Discriminant analysis (NCSS vers. 5.03, Hintze 1992) was used to examine
how the water quality variables as well as elevation, lake depth, and
lake surface area (independent variables) would predict the placement of
lakes into four classification categories (dependent variable) based on
the four vegetation zones. This was elucidated during the analysis by:
1) the construction of a classification matrix according to the
assignment of lakes to the classification categories; 2) determination
of classification accuracy by calculation of the percent reduction in
classification error due to the independent variables; and 3)
determination of the number of lakes misclassified. The discriminant
analysis also calculated three canonical variate scores for each lake,
and calculated the percent variation attributable to each variate, as
well as the correlations between each variate and each independent
variable. An initial analysis was performed using all independent
variables (Table 2.4). A second analysis was performed using only
independent variables found to have significant influence during the
first analysis.
Table 2.4. Identification of independent variables having significant influence during the initial discriminant analysis using all eleven variables.
| Variable | F-probability |
|---|---|
| Elevation | <0.001 |
| Surface Area | 0.301 |
| Depth | 0.184 |
| pH | <0.001 |
| Alkalinity | <0.001 |
| Total Kjeldahl-N | <0.001 |
| Ammonia-N | 0.113 |
| Nitrate-N | 0.011 |
| Total Phosphorus | 0.286 |
| Orthophosphate-P | 0.035 |
Chapter 2