CHAPTER 2
Physical and Chemical Characteristics of Lakes in the Glacially Influenced Landscape of the
North Cascades Mountain Range, Washington State, USA


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.

LakeElevation (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.

VariableMethodDetection
limits
(Units)

pHPortable 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
AlkalinityElectrometric titration to pH 4.50.2(mg/l)
ConductivityWheatstone Bridge, Yellow Spring model 33, corrected to 25°C0.4 (µS/cm)
Nitrate-NTechnicon Autoanalyzer, automated cadmium reduction0.001 (mg/l)
Kjeldahl-NNessler's Reagant finish 0.01(mg/l)
Ammonia-NTechnicon Autoanalyzer, colormetric automated phenate0.05(mg/l)
Total PhosphorusPersulfate digestion, ascorbic acid finish0.001(mg/l)
Orthophosphate-PReactive phosphate, ascorbic acid finish0.001(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.

VariableF-probability

Elevation<0.001
Surface Area0.301
Depth0.184
pH<0.001
Alkalinity<0.001
Total Kjeldahl-N<0.001
Ammonia-N0.113
Nitrate-N0.011
Total Phosphorus0.286
Orthophosphate-P0.035

Chapter 2


Abstract | Introduction | Study Area | Methods | Results | Discussion | Literature Cited


Chapter 1 | 2 | 3 | 4 | 5 | 6 | 7


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Last Updated: 01-Feb-2000