The Bacterial and Chemical Inputs to Zion National Park
J. Da in Maddox George E. Hart
Department of Forestry and Outdoor Recreation Utah State University Logan, Utah 84322
December, 1977
The Bacterial and Chemical Inputs to Zion National Park
J. Da in Maddox George E. Hart
Department of Forestry and Outdoor Recreation Utah State University Logan, Utah 84322
December, 1977
The Bacterial and Chemical Inputs to Zion National Park
J. Dain Maddox George E. Hart
Department of Forestry and Outdoor Recreation Utah State University Logan, Utah 84322
December, 1977
Digitized by the Internet Archive
in 2012 with funding from
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Table of Contents
List of Tables iii
List of Figures v
Abstract vi
Introduction 1
Previous Investigations 2
Sampling Methods 4
Study Area 4
North Fork Watershed 6
East Fork Watershed 7
LaVerkin Watershed 9
Sampling Sites 9
Parameters Measured 9
Equipment Used 11
Analysis of Data 11
Results and Discussion 12
Bacterial Results 12
Bacterial Discussion 18
Chemical Results ..... 20
Conclusions and Recommendations 28
Appendix 31
Ill
List of Tables
Page
Table 1. Drainage basin areas to the North Fork of the
Virgin River and East Fork of the Virgin River and
LaVerkin Creek 4
Table 2. Land ownership of the North Fork of the Virgin River above the Zion National Park Headquarters (BLM, 1975) 7
Table 3a. Total col i form concentrations for the upstream,
boundary, and headquarter sampling stations (3 repli- cates of one sample were analyzed for each date) ... 13
Table 3b. Fecal col i form concentrations for the upstream,
boundary, and headquarter sampling stations (3 repli- cates of one sample were analyzed for each date) ... 14
Table 3c. Fecal streptococcus concentrations for the upstream, boundary and headquarter sampling stations (3 repli- cates of one sample were analyzed for each date) ... 15
Table 4. Mean bacteria concentrations with percent increases
for the upstream and boundary sampling stations ... 16
Table 5. Group comparison of means and associated confidence levels for the upstream and boundary sampling stations 16
Table 6. Bacteria concentrations for the East Fork of the Virgin River as measured near the North Fork confluence 17
Table 7. Bacteria concentrations for LaVerkin Creek as
measured at Lee's Pass Trail 17
Table 8. Water quality standards for swimming water, Utah
State Division of Health (1975) 19
Table 9. Water quality data for the North Fork of the Virgin
River near the Park Headquarters 21
Table 10. Recommended upper limits of chemical concentrations for swimming and fishery waters (McKee and Wolfe, 1963) 22
IV
Page
Table 11. Water quality data for LaVerkin Creek near LaVerkin,
Utah and at Lee's Pass Trail 23
Table 12. Water quality data for the East Fork of the Virgin River near the confluence with the North Fork of the Virgin River 25
Table 13. Water chemistry data for the North Fork of the Virgin rtiver as measured at the headquarters and Chamberlain's Ranch, July 23, 1976 26
List of Figures
Page
Figure 1. The three major drainage basins of Zion National Park: North Fork of the Virgin River, East Fork of the Virgin River, and LaVerkin Creek .... 5
Figure 2. The location of the upstream and boundary sampling sites on the North Fork of the Virgin River 8
Figure 3. The chemical and bacterial sampling sites for the
North Fork, East Fork, and LaVerking Creek .... 10
VI
Abstract
Three major streams flow through Zion National Park: the North Fork of the Virgin River, the East Fork of the Virgin River, and LaVerkin Creek. The water quality of these three streams was studied during the summer of 1977. Bacterial indicators and the background water chem- istry were measured.
Given the location and frequency of the recreational use of the Park, emphasis was placed on the bacterial concentrations of the North Fork. Water samples were taken both inside and outside the Park to determine bacterial inputs of surrounding areas. It is shown that some upstream uses on private land do have an impact on water quality in the North Fork.
Introduction
Zion National Park is drained by three major streams, the North and East Fork (of the Virgin River) and LaVerkin Creek. The headwaters of all three streams are located outside the Park. Because the water quality of these streams has been determined in part by land use outside the Park, this study was designed to monitor the water quality entering the Park, and, when possible, to study key areas of water quality degra- dation outside the Park. The study includes the analysis of both the water chemistry and bacteriology of the three major streams. Emphasis was given to the North Fork because of its heavier recreational use.
Study objectives
1) To determine the bacterial water quality of the North Fork as it enters Zion National Park.
2) To evaluate land use practices outside the Park as they may influence the water quality of the North Fork.
3) To establish water chemistry baseline data for the North Fork, East Fork and LaVerkin Creek during summer low flows.
4) To present conclusions and recommendations.
Previous Investigations
Nonpoint sources of pollution are receiving increased attention in wildland water quality management. One of the primary sources of non- point bacterial pollution comes from domestic animal grazing. Cattle and sheep grazing contribute to increases in bacterial concentrations of mountain streams; however, the magnitude of this increase varies greatly.
One of the primary factors affecting bacterial inputs is the prox- imity of the grazing animal to the live stream channel. Kunkle (1970) found that increases in bacterial levels of mountain streams were directly related to the accessability of cattle to the stream. Similar results were found in studies by Morrison and Fair (1966) and Kunkle and Me i man (1967).
In addition to the accessability factor, the simple presence of grazing animals influences wildland water quality. Darling and Coltharp (1973) found significant increases in bacteria concentration in streams directly downstream from cattle and sheep grazing. Skinner et al. (1972) showed a strong correlation between grazing periods and increased bacterial numbers within high mountain watersheds.
There seems little question that grazing does have an impact on wildland water quality; however, there are other factors to be considered, First, Watler and Bottman (1967), and Stuart et al. (1971) have shown that wildlife can also cause increases in stream bacteria levels.
Second, Mack (1974) has demonstrated that bacteria can survive and even multiply in natural waters. This factor complicates the accurate measurement of bacterial inputs—regardless of the nonpoint source. Third, Buckhouse (1975) showed that bacterial life spans can be greatly influenced by the conditions of cattle feces. If the feces are allowed to dry quickly, the associated bacteria become encased within a protective media and may survive there for several years. These all add to the complexity of evaluating the impact of grazing on wildland water quality.
In addition to the above considerations, some bacterial indicators are better than others for monitoring the impact of domestic animal wastes on water quality. Kunkle (1977) used total coliform (TC), fecal streptococci (FS), enterococci and fecal coliform (FC) as the primary indicator organisms. Using a controlled environment, Kunkle found the fecal col i forms to be the most responsive and accurate measurement of cattle feces contamination of wildland waters.
Sampling Methods
During the summer of 1977 three streams were sampled. Each has headwaters outside Zion National Park and each represents a major surface water resource for the Park. This section discusses the study areas and reasons for their selection, the parameters measured, the sampling sites, the equipment used, and the analysis of data.
Study area
Figure 1 shows the location of Zion National Park with respect to the three drainage basins. The area of each of these watersheds is given in Table 1.
Table 1. Drainage basin areas for the North Fork and East Fork of the Virgin River and LaVerkin Creek.
Drainage basin Area (miles )
North Fork 364
East Fork 328
LaVerkin Creek 41
The southwestern section of the Park shows no drainage network. This section has not yet been studied for water quality. The area consists primarily of ephemeral streams with their headwaters located totally within the Park boundaries.
Scale i:2so,ooo q 5
10
Statute miles
Figure 1. The three major drainage basins of Zion National Park: the North Fork of the Virgin River, the East Fork of the Virgin River, and LaVerkin Creek.
North Fork Watershed
The North Fork watershed receives the heaviest visitor use of the three drainages. This visitor use is restricted to the narrow canyon bottom and consists primarily of sightseeing, camping, and stream channel hiking. Flash flood threats and low water temperatures often restrict recreational water use to mid and late summer periods. These periods usually coincide with the periods of grazing use upstream of the park boundary.
This watershed represents a mosaic of land ownerships (Table 2). Private lands total 65 percent of the watershed, all of which lie upstream from Zion National Park. The most frequent land uses include cattle grazing, summer homes, and private hunting clubs.
This study measured the impact of cattle grazing on the water quality of the North Fork. Two sampling sites were located on the North Fork, one at the park boundary and another 2.5 miles upstream (Figure 2). The cattle grazing within this 2.5 mile reach is confined to narrow pas- ture lands adjacent to the North Fork. The cattle have free access to the stream.
Table 2. Land ownership of the North Fork of the Virgin River above the Zion National Park Headquarters (BLM, 1975).
|
Percent of total area |
Mi2 |
||
|
Private Land |
65 |
236 |
|
|
State Land |
3 |
10 |
|
|
Federal Land |
|||
|
National Park Service |
21 |
78 |
|
|
Bureau of Land Management |
9 |
32 |
|
|
U.S. Forest Service |
2 |
8 |
|
|
TOTAL |
100 |
364 |
East Fork Watershed
From a water quality perspective, the East Fork is the most complex of the three drainages. As can be seen from Figure 1, the drainage basin encompasses several small communities. These communities and their associated agricultural and livestock holdings are adjacent to the East Fork of the Virgin River. After passing through these com- munities, the East Fork flows through the most primitive and inaccessable section of the Park, Parunuweap Canyon. Thus, the drainage basin receives heavier use outside the Park than within the Park.
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LaVerkin Watershed
Like the North Fork, LaVerkin Creek drains private lands before entering National Park Service land. Here the private land use consists of cattle and sheep grazing. Grazing occurs between April and October and as many as 300 head of cattle and 600 head of sheep may be grazing per season within the basin headwaters (Greely 1977).
This area of the Park is referred to as the Kolob Section. Visitor use is light, compared to the North Fork section of the Park. Also, unlike the North Fork, visitors are not restricted to the active stream channel; they have much greater flexibility in selecting areas of use.
Sampling sites
Five sites were sampled: three on the North Fork and one each on
the East Fork and LaVerkin Creek. The East Fork, LaVerkin Creek, and
one of the North Fork sampling sites were located within Zion National
Park. These sites were designed to measure the water chemistry and
bacteria levels of the water resources within the Park. The remaining
two sites on the North Fork were located outside the Park and were chosen
to measure the bacterial inputs into the Park from upstream use. These
two sites were located above and below specific land uses, as shown in Figure 3.
The parameters measured
Three bacterial indicators were measured: total col i forms (TC), fecal coliforms (FC), and fecal streptococci (FS). The physical parameters
10
x Chemical Sampling
O Bacterial Sampling
C Chemical and Bacterial Sampling
Scale 1:250,000 o 5
10
Statute miles
Figure 3. The chemical and bacterial samplings sites for the North Fork, East Fork, and LaVerkin Creek.
11
included turbidity and total dissolved solids. A broad spectrum of chemical elements were analyzed in addition to conductivity, alkalinity and total hardness.
Equipment used
The membrane filter technique was used for all bacterial analysis. Incubators, sample bags, filter holders, filter papers and procedures were used in accordance with Standard Methods 14th Edition (1976). M-FC and M-Endo growth mediums were taken from prepared ampules and used for the FC and TC incubations, respectively. M-enterococcus agar was used in the incubation of the FS.
Analysis of data
The bacterial samples were collected between 9:00 a.m. and 12:00 noon and were processed at the Park headquarters within 12 hours after collection. Colony identification and plate count methods were followed as outlined in Standard Methods (1976). Standard blanks were taken of the buffer water, filter holders, filter pads, and petri dishes.
One sample was taken at each site. From this sample, three replicates were taken for each of the bacterial indicators. This was done to determine the proper sample volume necessary to achieve the optimum plate count (Standard Methods 1976).
The chemical analyses, including conductivity and turbidity, were' performed at Ford Chemical Laboratory in Salt Lake City. These samples were iced during transport and were delivered to Ford Laboratory within 24 hours after their collection.
12
Results and Discussion
Bacterial results
The results of the analysis for the three stations on the North Fork are given in Tables 3a, b, and c. For all three tables, bacterial concentrations are given for the boundary, the upstream and the head- quarter locations. The total and fecal coliform concentrations measured at the upstream station were greater than the concentrations measured at the headquarters station (Table 3a and 3b). Table 3c shows a similar trend for the fecal strep concentrations.
Table 4 gives the mean concentration of the three bacterial indicators for the upstream and boundary stations. The percent increase in bacterial concentrations was then calculated using these means. The TC increase was the largest, 526 percent, and the FS increase was the lowest, 216 percent.
A group comparison of the mean bacterial concentrations was cal- culated for the upstream and boundary stations. This analysis indicates that the bacterial concentrations at the boundary station were greater than the bacterial concentrations at the upstream station. The con- centration means for the two stations were found to be significantly different at the 95 percent or higher confidence level (Table 5).
13
Table 3a. Total coliform concentrations for the upstream, boundary,
and headquarter sampling stations (3 replicates of one sample were analyzed for each date).
|
Bacteria |
concentrations (col |
onies/100 ml) |
|
|
Date |
Upstream |
Boundary |
Headquarters |
|
July 27, 1977 |
1,200 |
12,000 |
no sample taken |
|
28 |
1,600 |
14,600 |
10,700 |
|
29 |
120 |
5,300 |
no sample taken |
|
30 |
300 |
11,300 |
4,800 |
|
31 |
1,160 |
5,450 |
no sample taken |
|
Aug. 1, 1977 |
2,300 |
5,400 |
3,600 |
|
2 |
3,700 |
4,600 |
1,800 |
|
3 |
1,800 |
11,000 |
3,500 |
|
4 |
2,000 |
12,800 |
4,200 |
|
Sept. 2, 1977 |
1,320 |
10,700 |
3,800 |
|
3 |
1,100 |
7,600 |
3,200 |
|
4 |
1,200 |
10,300 |
2,800 |
14
Table 3b. Fecal coliform concentrations for the upstream, boundary
and headquarter sampling stations (3 replicates of one sample were analyzed for each date).
|
Bacteria |
concentrations (col |
onies/100 ml ) |
||
|
Date |
Upstream |
Boundary |
Headquarters |
|
|
July 27, 1977 |
0* |
400 |
no sample |
taken |
|
28 |
0* |
600 |
0* |
|
|
29 |
0* |
220 |
no sample |
taken |
|
30 |
100* |
200 |
0* |
|
|
31 |
35 |
1,300 |
no sample |
taken |
|
Aug. 1, 1977 |
90 |
200 |
60 |
|
|
2 |
80 |
100* |
80 |
|
|
3 |
320 |
420 |
120 |
|
|
4 |
360 |
460 |
140 |
|
|
Sept. 2, 1977 |
20* |
1,600 |
20* |
|
|
3 |
80* |
1,200 |
72 |
|
|
4 |
60 |
620 |
63 |
The colony count was below the optimum range recommended by the Millipore Company and is thus less reliable than other values.
15
Table 3c. Fecal streptococcus concentrations for the upstream,
boundary and headquarter sampling stations (3 replicates of one sample were analyzed for each date).
|
Bacteria |
concentrations (col |
onies/100 ml) |
|
|
Date |
Upstream |
Boundary |
Headquarters |
|
July 27, 1977 |
60 |
500 |
no sample taken |
|
28 |
100* |
1,000 |
160 |
|
29 |
80 |
700 |
no sample taken |
|
30 |
100* |
400 |
600 |
|
31 |
120 |
500 |
no sample taken |
|
Aug. 1, 1977 |
520 |
800 |
no |
|
2 |
400 |
600 |
200 |
|
3 |
240 |
700 |
180 |
|
4 |
280 |
760 |
230 |
|
Sept. 2, 1977 |
80* |
560 |
40 |
|
3 |
140 |
700 |
160 |
|
4 |
120 |
720 |
90* |
The colony count was below the optimum range recommended by the Mi Hi pore Company and is thus less reliable than other values.
16
Table 4. Mean bacteria concentrations with percent increases for the upstream and boundary sampling stations.
|
Bacteria concentration (colonies/100 ml) |
||
|
Bacteria |
Upstream |
Boundary |
|
TC |
1,480 |
9,270 |
|
FC1 |
127 |
680 |
|
FS |
190 |
600 |
Percent increase
526% 435% 216%
The sampling dates having "0" bacteria concentrations were not included in the mean calculations for either of the sampling locations.
Table 5. Group comparison of means and associated confidence levels for the upstream and boundary sampling stations.
|
Bacterial parameter |
Degrees of freedom |
Computed t |
Table t2 value at |
percent confidence level |
|
Total Col i form |
11 |
7.242 |
3.106 |
99% |
|
Fecal Col i form |
8 |
2.707 |
2.306 |
95% |
|
Fecal Strep. |
11 |
8.861 |
3.106 |
99% |
Dixon, Wilfrid J. and Massey, Frank J. 1969, Analysis. McGraw Hill, New York. p. 116.
Dixon and Massey, p. 464.
Introduction to Statistical
17
The East Fork and LaVerkin Creek were also sampled for bacterial concentrations. Tables 6 and 7 give the bacterial results for these two streams. Samples were taken at three dates at each of the locations. These results are presented as summer baseline data and are not intended to represent trends or absolute concentrations.
Table 6. Bacteria concentrations for the East Fork of the Virgin River as measured near South Park boundary.
Date
Bacteria Concentration (colonies/lOOml) TC FC FS
July 26, 1977 2,700 620 270
August 2, 1977 2,500 640 400
September 2, 1977 2,300 580 360
Table 7. Bacteria concentrations for LaVerkin Creek, as measured at Lee Pass Trail, 1977.
Date
Bacteria Concentration (colonies/ 100ml)
TC FC FS
July 27, 1977 2,120 60 240
August 2, 1977 1,400 360 200
September 3, 1977 1,600 420 280
18
Bacteria discussion
The large increases in bacterial concentrations over the 2.5 mile reach of the North Fork indicate that the current land use does have an impact on the water quality. The statistical analysis of this report indicates that the two sampling points represent different populations. From bacterial analysis and field observations, the cattle grazing between the upstream and boundary sampling points have the greatest single impact on the water quality of the North Fork as it enters Zion National Park.
Once within the park, the North Fork bacterial concentration becomes diluted by tributary inflows. Previous studies (Maddox, 1977) have shown the bacterial concentrations of Deep Creek and Kolob Creek to be substantially lower than the bacterial concentrations of the North Fork for any given sampling day. This dilution effect accounts for the lower bacterial concentrations for the headquarter station when compared to the boundary concentration.
In 1975, the Utah State Division of Health published its suggested water quality criteria for swimming waters (Table 8). The upstream and boundary bacteria concentrations for both TC and FC exceed these sug- gested upper limits. The headquarters bacterial concentrations exceed the upper limits for TC, but not for FC. LaVerkin Creek and East Fork also exceed the upper limits for both TC and FC.
19
Table 8. Water quality standards for swimming waters, Utah State Division of Health (1975).
Standard definition
Standard Number
Col i form Density (colony/ 100ml)
Fecal Col i form Density (colony/ 100ml)
Monthly mean may not exceed
1000
200
No more than 20% of samples collected in one month may exceed
1000
No more than 10% of samples collected in one month may exceed
4000
400
No more than 5% of samples collected in one month may exceed
4000
20
Chemical results
Table 9 gives the chemical analysis for the North Fork. The three samples were taken during the summer months over a three year period. The sampling dates ranged from late spring runoff (May) to early fall. These concentrations suggest that many of the chemical parameters remain relatively constant throughout the sampling periods. This indicates that as flows increase the chemical inputs increase proportionately, thus the concentrations remain relatively constant throughout the sampling periods. This indicates that as flows increase the chemical inputs increase proportionately, thus the concentrations remain relatively constant.
Table 10 gives the recommended upper limits for swimming and fishery waters for several chemical elements. Sodium (as Na) in the only chemical parameter exceeding these limits. This exceedence is true for the three sampling dates. Sodium is common in most wildland waters with concen- trations varying both locally and regionally. The human intake limits for sodium vary greatly, but unless the intake exceeds 1000 mg/1 (Water Quality Crtieria, 1972), there is little concern.
However, fisheries are more susceptable to high sodium concentrations. McKee and Wolfe (1963) have found 10 mg/1 concentration to be an acceptable upper limit for most fresh water fish.
Table 11 gives the water chemistry analysis for LaVerkin Creek. Three samples were taken during a single summer season. One sample was taken near the city of LaVerkin, the other two samples were taken within Zion National Park. Between the two sampling locations there are numerous agricultural lands, row crops, pasture lands, fruit trees, and
21
Table 9. Water quality data for the North Fork of the Virgin River near the Park headquarters.
|
Sample dates |
|||
|
water qua I ity |
|||
|
parameter Sept> 17> lg?5 |
July 23, 1976 |
May 16, 1977 |
|
|
Turbidity (JTU) |
4.2 |
20.0 |
2.00 |
|
Conductivity (ymhos/cm) |
793.0 |
820.0 |
900.0 |
|
PH |
7.14 |
7.56 |
7.81 |
|
Total dissolved solids |
|||
|
at 180°C. (mg/1) |
516.0 |
53r. |
600.0 |
|
Alkalinity as CaC03 (mg/1) |
158.0 |
234.0 |
168.0 |
|
Aluminum as Al (mg/1) |
<0.01 |
0.0/ |
0.071 |
|
Arsenic as As (mg/1) |
<0.01 |
0.008 |
<0.001 |
|
Bicarbonate as HCO3 (mg/1) |
191.49 |
202.5 |
204.9 |
|
Barium as Ba (mg/1) |
<0.01 |
^0.144 |
0.091 |
|
Boron as B (mg/1) |
<0.01 |
<0.001 |
0.22 |
|
Cadmium as Cd (mg/1 ) |
0.002 |
<0.001 |
<0.001 |
|
Calcium as Ca (mq/1) |
55.2 |
51.2 |
21.6 |
|
Carbonate as CO3 (mg/1) Chloride as CI (mg/1) |
<0.01 |
<0.01 |
<0.01 |
|
88.0 |
90.0 |
130.0 |
|
|
Chromium as Cr (Hex) (mg/1) |
<0.01 |
<0.001 |
<0.001 |
|
Cyanide as Cn (mg/1) |
<0.01 |
<0.01 |
<0.01 |
|
Copper as Cu (mg/1) |
0.02 |
0.006 |
0.007 |
|
Fluoride as F (mg/1) |
0.13 |
0.32 |
0.28 |
|
Total Hardness as CaC03 |
|||
|
(mg/1) |
250.0 |
234.0 |
230.0 |
|
Iron (Total) as Fe (mg/1) |
0.15 |
0.120 |
0.086 |
|
Iron (Filtered) as Fe (mg/1) |
0.02 |
0.100 |
0.050 |
|
Lead as Pb (mg/1) |
<0.01 |
0.005 |
<0.001 |
|
Magnesium as Mg (mg/1) |
26.88 |
25.4 |
42.24 |
|
Manganese as Mn (mg/1) |
0.01 |
0.035 |
0.034 |
|
Mercury as Hg (mg/1) |
<0.001 |
<0.0002 |
<0.0002 |
|
Nitrate as NO3-N (mg/1) |
0.04 |
0.02 |
0.10 |
|
Phosphate as PO* (mg/1) Potassium as K (mg/1) |
0.100 |
0.065 |
0.035 |
|
3.69 |
3.32 |
3.14 |
|
|
Selenium as Se (mg/1) |
<0.01 |
0.077 |
<0.001 |
|
Silica as Si02 (mg/1) |
4.15 |
9.9 |
21.5 |
|
Silver as Ag (mg/1) |
0.007 |
<0.001 |
<0.001 |
|
Sulfate as SOa (mg/1) Sodium as Na (mg/1) |
85.50 |
92.0 |
82.0 |
|
57.00 |
73.0 |
122.50 |
|
|
Zinc as Zn (mg/1) |
0.01 |
0.007 |
0.042 |
22
Table 10. Recommended upper limits of chemical concentrations for swimming and fishery waters (McKee and Wolfe, 1963).
Chemical parameter
Recommended upper limit
Aluminum as Al (mg/1) Arsenic as As (mg/1 ) Barium as Ba (mg/1) Boron as B (mg/1 ) Cadmium as Cd (mg/1) Calcium as Ca (mg/1) Chloride as CI (mg/1) Chromium as Cr (Hex) (mg/1) Cyanide as Cn (mg/1) Copper as Cu (mg/1) Fluoride as F (mg/1) Iron (Total) as Fe (mg/1) Iron (Filtered) as Fe (mg/1) Lead as Pb (mg/1) Magnesium as Mg (mg/1) Manganese as Mn (mg/1) Mercury as Hg (mg/1) Nitrate as NO3-N (mg/1) Phosphate as P0*-P fmg/l ) Potassium as K (mg/1 ) Selenium as Se (mg/1) Silica as SiOo (mg/1) Silver as Ag tmg/1) Sulfate as SOa (mg/1) Sodium as Na (mg/1) Zinc as Zn (mg/1)
0.50 0.10 5.00
1000.00 1500.00 5.00 0.05 0.10 5.0 0.20
0.10 100.0 40.0
0.004
4.20 15.00 50.00
2.0 50.0
0.033 500.00 10.06
0.10
Conductivity (ymhos/cm at 25°C)
2000.00
23
Table n. Water quality data for La Verkin Creek near La Verkin, Utah and at Lee's Pass Trail.
|
Sampl |
e location and |
date |
|
|
Water quality parameter M |
LaVerkin |
Lee's Pi |
iss Trail |
|
ay 16, 1977 |
Aug. 5, 1977 |
Sept. 4, 1977 |
|
|
Turbidity (JTU) |
3.0 |
1.5 |
2.0 |
|
Conductivity (^mhos/cm) |
1,670.0 |
677.0 |
655.0 |
|
PH |
7.62 |
7.97 |
7.80 |
|
Total dissolved solids |
|||
|
at 180°C. (mg/1) |
1,105.0 |
432.0 |
422.0 |
|
Alkalinity as |
|||
|
CaC03 (mg/1) Aluminum as Al (mg/1) |
180.0 |
148,0 |
152.0 |
|
0.043 |
0.063 |
0.149 |
|
|
Arsenic as As (mg/1) |
<0.001 |
<0.001 |
<0.001 |
|
Bicarbonate as HCO, (mg/1) Barium as Ba (mg/1 J |
219.6 |
180.6 |
185.4 |
|
0.048 |
0.063 |
0.184 |
|
|
Boron as B (mg/1) |
0.22 |
0.15 |
0.04 |
|
Cadmium as Cd (mg/1) |
<0.001 |
<0.001 |
<0.001 |
|
Calcium as Ca (mg/1) |
86.4 |
84.8 |
80.8 |
|
Carbonate as CO3 (mg/1) Chloride as CI (mg/1) |
<0.01 |
<0.01 |
<0.01 |
|
16.0 |
8.0 |
10.0 |
|
|
Chromium as Cr (Hex) (mg/1) |
<0.001 |
<0.001 |
<0.001 |
|
Cyanide as Cn (mg/1) |
<0.01 |
<0.01 |
<0.01 |
|
Copper as Cu (mg/1) |
0.005 |
0.002 |
0.004 |
|
Fluoride as F (mg/1) |
0.40 |
0.20 |
0.15 |
|
Total Hardness as CaC03 |
|||
|
(mg/1) |
486.0 |
330.0 |
336.0 |
|
Iron (Total) as Fe (mg/1) |
0.096 |
0.069 |
0.133 |
|
Iron (Filtered) as Fe (mg/1) |
0.044 |
0.040 |
0.100 |
|
Lead as Pb (mg/1) |
<0.001 |
<0.001 |
<0.001 |
|
Magnesium as Mg (mg/1) |
64.8 |
2.3293 |
32.16 |
|
Manganese as Mn (mg/1) |
0.027 |
0.004 |
0.007 |
|
Mercury as Hg (mg/1) |
<0.0002 |
<0.0002 |
<0.0002 |
|
Nitrate as NO3-N (mg/1) |
0.36 |
0.010 |
<0.01 |
|
Phosphate as POa (mg/1) Potassium as K (mg/1) |
0.045 |
0.010 |
0.01 |
|
2.93 |
2.653 |
3.70 |
|
|
Selenium as Se (mg/1) |
<0.001 |
<0.001 |
<0.001 |
|
Silica as SiOo (mg/1) Silver as Ag (mg/1) |
26.0 |
7.0 |
8.0 |
|
0.005 |
0.014 |
<0.001 |
|
|
Sulfate as SO4 (mg/1) |
580.0 |
202.0 |
194.0 |
|
Sodium as Na (mg/1) |
143.0 |
17.10 |
11.93 |
|
Zinc as Zn (mg/1 ) |
0.025 |
0.006 |
0.033 |
24
grain crops. Conductivity, total dissolved solids, total hardness, magnesium, sulfate and sodium all show marked increases. However, these increases cannot be totally attributed to agricultural use. The dif- ferent dates of sampling and subsequent flow volumes may have an impact on these water chemistry variations.
With the exception of sodium, the water samples taken within the Park (Lee's Pass Trail) are within the recommended limits shown in Table 10. Sodium again exceeds this limit, but, as stated above, this becomes of concern only to fresh water fisheries. In this case, the LaVerkin Creek samples are only slightly above the recommended limit and would probably have little, if any, impact on the fisheries.
Table 12 gives the water chemistry for the East Fork. The two samples were taken in the summer of 1977 just upstream from the confluence of the East Fork and the North Fork. These results represent the upstream water use of the East Fork by the municipal and agricultural users in Glendale, Orderville, Mt. Carmel and Mt. Carmel Junction. In comparing these data with the recommended limits of Table 10, the sodium concen- tration once again exceeds the recommended limit.
The water chemistry of the North Fork changes as it flows through the Park. Table 13 illustrates the magnitude of the downstream change for one sampling day. On this particular day, 21 of the 34 chemical parameters increased, 8 remained unchanged, and 5 decreased in concen- tration. There are numerous variables that may account for these changes, not the least of which is the tributary inflow. The concentrations
25
Table 12. Water quality data for the East Fork of the Virgin River near the confluence with the North Fork of the Virgin
River.
|
Water quality |
Sampling |
dates |
|
parameter |
May 13, 1977 |
Aug. 5, 1977 |
|
Turbidity (JTU) |
2.50 |
1.6 |
|
Conductivity (ymhos/cm) |
600.0 |
490.0 |
|
PH |
7.73 |
8.10 |
|
Total Dissolved Solids at |
||
|
180° C. (mg/1) |
400.0 |
316.0 |
|
Alkalinity as CaCOq (mg/1) Aluminum as Al (mg/1) |
150.0 |
148.0 |
|
0.025 |
0.113 |
|
|
Arsenic as As (mg/1) |
<0.001 |
<0.001 |
|
Bicarbonate as HCO? (mg/1) Barium as Ba (mg/lj |
183.0 |
180.6 |
|
0.038 |
0.040 |
|
|
Boron as B (mg/1) |
0.14 |
0.17 |
|
Cadmium as Cd (mg/1) |
<0.001 |
<0.001 |
|
Calcium as Ca (mg/1) |
28.0 |
55.2 |
|
Carbonate as CO3 (mg/1) Chloride as CI (mg/1) |
<0.01 |
<0.01 |
|
24.0 |
24.0 |
|
|
Chromium as Cr (Hex) (mg/1) |
<0.001 |
<0.001 |
|
Cyanide as Cn (mg/1) |
<0.01 |
<0.01 |
|
Copper as Cu (mg/1) |
0.003 |
0.002 |
|
Fluoride as F (mg/1) |
0.35 |
0.17 |
|
Total Hardness as CaC(h (mg/1) Iron (Total) as Fe (mg/1) |
220.0 |
230.0 |
|
01079 |
0.125 |
|
|
Iron (Filtered) as Fe (mg/1) |
0.050 |
0.100 |
|
Lead as Pb (mg/1) |
<0.001 |
<0.001 |
|
Magnesium as Mg (mg/1) |
36.0 |
22.08 |
|
Manganese as Mn (mg/1 ) |
0.009 |
0.007 |
|
Mercury as Hg (mg/1) |
<0.0002 |
<0.0002 |
|
Nitrate as NO3-N (mg/1) Phosphate as P0* (mg/1) Potassium as K (mg/1) |
0.70 |
0.70 |
|
0.045 |
0.010 |
|
|
2.97 |
3.57 |
|
|
Selenium as Se (mg/1) |
<0.001 |
0.003 |
|
Silica as SiO? (mg/1) Silver as Ag (mg/1) |
22.0 |
8.0 |
|
<0.001 |
<0.001 |
|
|
Sulfate as SOa (mg/1) Sodium as Na (mg/1) |
97.0 |
98.0 |
|
30.30 |
24.38 |
|
|
Zinc as Zn (mg/1) |
0.020 |
0.008 |
26
Table 13. Water chemistry data for the North Fork of the Virgin River as mea- sured at the headquarters and Chamberlain's Ranch, July 23, 1976.
|
Sampling lo |
cation |
|
|
Parameter |
Chamberlain's Ranch |
Gage |
|
Turbidity (JTU) |
15.0 |
20.0 |
|
Conductivity (ymhos/cm) |
570.0 |
820.0 |
|
PH |
7.60 |
7.56 |
|
Total dissolved solids at |
||
|
180°C. (mg/1) |
370.0 |
535.0 |
|
Alkalinity as CaC03 (mg/1) |
206.0 |
234.0 |
|
Aluminum as Al (mg/1) |
0.065 |
0.070 |
|
Arsenic as As (mg/1) |
<0.001 |
0.008 |
|
Bicarbonate as HCOq (mg/1) Barium as Ba (mg/l) |
251.3 |
202.5 |
|
0.089 |
0.144 |
|
|
Boron as B (mg/l) |
<0.001 |
<0.001 |
|
Cadmium as Cd (mg/l ) |
<0.001 |
<0.001 |
|
Calcium as Ca (mg/l ) |
47.2 |
51.2 |
|
Carbonate as CO3 (mg/l) Chloride as CI (mg/l) |
<0.01 |
<0.01 |
|
4.0 |
90.0 |
|
|
Chromium as Cr (Hex) (mg/l) |
<0.001 |
<0.001 |
|
Cyanide as Cn (mg/l) |
<0.01 |
<0.01 |
|
Copper as Cu (mg/l) |
0.005 |
0.006 |
|
Fluoride as F (mg/l) |
0.30 |
0.32 |
|
Total Hardness as CaC03 (mg/l) |
208.0 |
234.0 |
|
Iron (Total) as Fe (mg/l) |
0.110 |
0.120 |
|
Iron (Filtered) as Fe (mg/l) |
0.100 |
0.100 |
|
Lead as Pb (mg/l) |
<0.001 |
0.005 |
|
Magnesium as Mg (mg/l) |
21.6 |
25.4 |
|
Manganese as Mn (mg/l) |
0.025 |
0.035 |
|
Mercury as Hg (mg/l) |
<0.0002 |
<0.0002 |
|
Nitrate as NO3-N (mg/l) Phosphate as PCM (mg/l) Potassium as K (mg/l) |
0.05 |
0.02 |
|
0.035 |
0.065 |
|
|
1.62 |
3.32 |
|
|
Selenium as Se (mg/l J Silica as SiO? (mg/l) Silver as Ag (mg/l ) |
0.007 15.0 |
0.077 9.9 |
|
<0.001 |
<0.001 |
|
|
Sulfate as SO* (mg/l) Sodium as Na (mg/l) |
18.7 |
92.0 |
|
18.7 |
73.0 |
|
|
Zinc as Zn (mg/l) |
0.012 |
0.007 |
27
given in Table 13 serve to indicate possible directions of water chem- istry changes with respect to time and location. These concentrations offer baseline water chemistry data.
28
Conclusion and Recommendations
The following conclusions are the result of analyses of samples collected during the summers of 1976 and 1977.
1) The total col i form and fecal col i form concentrations of the North Fork of the Virgin River, the East Fork of the Virgin River, and LaVerkin Creek all exceed the Utah State Division of Health recommended limits for swimming waters.
2) The bacterial concentrations within Zion National Park are influenced more by the uses outside the Park than the uses within the Park.
3) Cattle grazing, adjacent and upstream from the Park, does have an impact on the bacterial concentrations of the North Fork of the Virgin River.
4) Over a 2.5 mile reach of the North Fork of the Virgin River total col i form, fecal coliform and fecal streptococcus increased
526, 435 and 216 percent, respectively. These increases are attributed primarily to cattle grazing within the 2.5 mile reach outside the park.
5) With the exception of sodium, all of the measured chemical element concentrations were within the recommended limits for fresh water fisheries.
6) Because of the bacterial concentrations, recreationists should be made aware of the potential health hazards of human injestion of the waters of the North Fork, East Fork, and LaVerkin Creek.
29
Literature Cited
American Public Health Association. 1976. Standard Methods for the Examination of Water and Wastewater. 14th ed. American Public Health Association, Inc., New York.
Buckhouse, John C. 1975. Water quality impact of burning and grazing on a chained pinyon-juniper site in southeastern Utah. Ph.D. dissertation, Utah State University, Logan, Utah.
Darling, L. A., and G. B. Coltharp. 1973. Effects of livestock grazing on the water quality of mountain streams. J_n: Proc. Symposium Water-Animal Relationships. Southern Idaho State College, Twin Falls, Idaho. June 1973:1-8.
Dixon, Wilfrid J., and Frank J. Massey, Jr. Introduction to Statistical Analysis. 3rd ed. McGraw Hill, New York, New York.
Environmental Protection Agency. 1972. Water quality criteria. Superintendent of Documents, U.S. Government Printing Office, Washington, D.C.
Greely, Hal. District Ranger, Zion National Park, Sprincjdale, Utah. Personal Communication, August 1, 1977.
Kunkle, S. H. 1970. Sources and transport of bacterial indicators
in rural streams. Presented at a symposium on the Interdisciplinary Aspects of Watershed Management, Montana State University, Bozeman, Montana. 3-6 August.
Kunkle, S. H. 1977. Using bacteria to monitor the influence of cattle wastes on water quality. (Unpublished).
Kunkle, S. H., and J. R. Meiman. 1967. Water quality of mountain water- sheds. Hydrology Paper No. 21, Colorado State University, Fort Collins, Colorado.
McKee, J. E., and H. W. Wolf. 1963. Water Quality Criteria. California State Water Resources Control Board. California.
Mack, W. N. 1974. Investigations into occurrence of coliform organisms from pristine streams. Dept. of Microbiology and Public Health, Michigan State University, East Lansing, Michigan. (Unpublished data).
Maddox, J. D. 1977. Water Resource Inventory of Zion National Park. M.F. paper, Utah State University, Logan, Utah
30
Morrison, S. M. , and J. F. Fair. 1966. Influence on environment on stream microbial dynamics, Hydrology Paper No. 13, Colorado State University, Fort Collins, Colorado.
Stuart, D. G. , G. K. Bissonnette, T. D. Goodrich, and W. G. Walter. 1971. Effects of multiple use on water quality of high mountain watersheds: Bacteriological investigations of mountain streams. Journal of Applied Microbiology 22:1048-1054.
U.S. Department of Interior, Bureau of Land Management. 1976. State of Utah, Land Ownership and Public Management Map, Dixie-S.
Utah State Division of Health. 1976. Standards of quality for waters of the state. Utah.
Walter, W. G. , and R. P. Bottman. 1967. Microbiological and chemical studies of an open and a closed watershed. Journal of Environmental Health 30:157-163.
31
Appendix A
Chemical analysis of Zion National Park water resources as analyzed by Ford Chemical Laboratory, Inc. Salt Lake City, Utah
32
Name
LABORATORY, INC.
Bacteriological and Chemical Analysis 40 WEST LOUISE AVENUE SALT LAKE CITY, UTAH 841 15 PHONE 485-5761
Mr. George; Hart
Address _ Forestry & Outdoor Recreation Utah State University Logan, UT 84321
Date: October 6, 1975
CERTIFICATE OF ANALYSIS
75-4199
jamp|e Water from North Fork of Virgin River at Highway 89 received on September 17 , 1975.
"urbidity
Conductivity
>H
"otal Dissolved Solids it 180° C.
alkalinity as CaCOs
Aluminum as Al
Arsenic as As
bicarbonate as HC03
barium as Ba
boron as B
admium as Cd
alcium as Ca
arbonate as CCX
hloride as CI
hromium as Cr (Hex)
yanide as Cn
opper as Cu
4.2
793.0
7.14
516.0
158.0
<0.01
0.02
it
JTU
.umhos/cm
_mg/ _mg/ <Q.Q1 mg/
<0.01 mg/
191.49
-mg/ -mg/
<^± mg/
°-002 mg/
55-2 mg/
<\0j_9J___mg/ 88. 0 mg/
<0-01 mg/
<0.01
mg/ mg/
Fluoride as F
Total Hardness as CaCOs
Iron (Total) as Fe
Iron (Filtered) as Fe
Lead as Pb
Magnesium as Mg
Manganese as Mn
Mercury as Hg
Nitrate as NO, — N
Phosphate as PO4
Potassium as K
Selenium as Se
Silica as Si02
Silver as Ag
Sulfate as SO*
Sodium as Na
Zinc as Zn
0.13
250.0
0.15
0.02
<0.01
26.88
0.01
— mg/1
— mg/' — mg/' — mg/' — mg/'
_mg/l
—mg/l <0.001 mg/i
0-04' mg/1
0.100 mg/1
3.69 mg/1
<0.01 mg/1
4-15 mg/]
O-OO"7 mg/1
9 5.50 mg/1
57.00 mg/1
0.01
-mg/1
r
^0^^%/^
Ford Chemical Laboratory, Inc.
33
LABORATORY, INC.
Bacteriological and Chemical Analysis 40 WEST LOUISE AVENUE SALT LAKE CITY, UTAH 84115 PHONE 485-5761
re:
August 17, 197 6
Jame
ample
Utah State University
ATTN: George Hart address Forestry Science Laboratory
CERTIFICATE OF ANALYSIS
76-5008
Logan, UT 84321
Water at North Fork-Virgin River, Chamberlin Ranch Received on July 23, 1976 - Zion Park Research:
urbidity
Conductivity
H
otal Dissolved Solids t 180° C.
Jkalinity as CaCOi
Juminum as Al
Tsenic as As
icarbonate as HCOs
arium as Ba
oron as B
admium as Cd
alcium as Ca
arbonate as COs
hloride as CI
hromium as Cr (Hex)
yanide as Cn
opper as Cu
15.0
JTU
0.30
570..Q umhos/cm
7.60
370.0
206.0
_mg/
_mg/ 0.065 mg/
CO. 001 mg/
2 51.3 mg/ 0-089 mg/
^0.001 mg/
Ao.003 mg/
4 7.2 mg/
<0.01 mg/
4_^0 mg/
cJKQQl mg/
<C0.01 mg/
0-005 mg/
208.0
0.100
Fluoride as F
Total Hardness as CaCOs
Iron (Total) as Fe
Iron (Filtered) as Fe
Lead as Pb v
Magnesium as Mg
Manganese as Mn
Mercury as Hg
Nitrate as NO, -N
Phosphate as PO<
Potassium as K
Selenium as Se
Silica as Si02
Silver as Ag
Sulfate as SOj
Sodium as Na
Zinc as Zn 0.012
_ mg/ — mg/
0.110 mg/
— mg/
0.001 mg/
21 . 6 mg/
0.025 mg/
<Q.Q0Q2 mg/
0.05 mg/
0. 035 mg/
1 . 62 mg/
0.007 mg/
15.0 mg/
^0.001 mg/
34.0 mg/
18.7 mg/
-mg/
r^^_
Ford Chemical Laboratory, Inc.
34
LABORATORY, INC.
Bacteriological and Chemical Analysis 40 WEST LOUISE AVENUE SALT LAKE CITY, UTAH 84115 PHONE 485-5761
Date:
August 17, 1976
pnwfl Utah State University
ATTN: George Hart Address Forestry Science Laboratory
Logan, UT 84321
CERTIFICATE OF ANALYSIS
76-5010
iample Water labeled Deep Creek Received on July 23 , 1976, Zion Park Research:
urbidity
Conductivity
>H
otal Dissolved Solids it 180° C.
alkalinity as CaCOs
Uuminum as Al
arsenic as As
bicarbonate as HCOs
•arium as Ba
toron as B
admium as Cd
alcium as Ca
arbonate as COs
hloride as CI
hromium as Cr (Hex)
yanide as Cn
opper as Cu
7.5
JTU
630.0 umhos/cm
7.58
410.0
138.0
-mg/1
mg/1
0-130 mg/1
^°'001 mg/1
168.4 mg/1
0-089 mg/i
<0.001 mg/1
0.002 mg/1
45.6 mg/i
^sO.01 mg/1
4 • 0 mg/1
^.Q.QQJ mg/1
j.0.01 mg/1
0.005 mg/i
Fluoride as F
Total Hardness as CaCOs
Iron (Total) as Fe
Iron (Filtered) as Fe
Lead as Pb
Magnesium as Mg
Manganese as Mn
Mercury as Hg
Nitrate as NO.-N
Phosphate as PCX
Potassium as K
Selenium as Se
Silica as Si02
Silver as Ag
Sulfate as SCX
Sodium as Na
Zinc as Zn
0.27
— mg/
180-0 mg/
&110 mg/
0-lOQ mg/
^0-001 mg/
15'84 mg/
Q-038 mg/
< 0.0002 mg/
< 0.01 mg/
0.035 mg/
— mg/
1.58
0.006
-mg/
Q.9Q mg/
<0.001 mg/
130.0 mg/
45.0 mg/
0-008 mg/
£ ^
Ford Chemical Laboratory, Inc.
35
LABORATORY, INC.
Bacteriological and Chemical Analysis 40 WEST LOUISE AVENUE SALT LAKE CITY, UTAH 84115 PHONE 485-5761
Date:
August 17, 1976
Utah State University
same
ATTN: George Hart
address Forestry Science Laboratory Logan, UT 84321
CERTIFICATE OF ANALYSIS
76-5009
ample Water Labeled Kolob Creek Received on July 23, 1976-Zion Park Research;
urbidity
Conductivity
iH
otal Dissolved Solids t 180° C.
Jkalinity as CaCOs
Jurninum as Al
trsenic as As
icarbonate as HCOs
arium as Ba
oron as B
admium as Cd
alcium as Ca
arbonate as CO3
hloride as CI
hromium as Cr (Hex)
yanide as Cn
opper as Cu
8.0
480.0
7.70
315.0
158.0
0.060
^.0.001
X92.8
0.099
<0.001
<0.001
50.4
<0.01
A^Q_
40.QQ1
^0.01
Q.Q11
JTU -umhos/cm
_mg/ _mg/ -mg/ -mg/ .mg/ .mg/ .mg/ -mg/ -mg/ .mg/ -mg/ .mg/ -mg/ .mg/
Fluoride as F
Total Hardness as CaCOs
Iron (Total) as Fe
Iron (Filtered) as Fe
Lead as Pb
Magnesium as Mg
Manganese as Mn
Mercury as Hg
Nitrate as NO, — N
Phosphate as PO«
Potassium as K
Selenium as Se
Silica as Si02
Silver as Ag
Sulfate as SO*
Sodium as Na
Zinc as Zn
0.30
190.0
0.080
0.050
0.030
-mg/ -mg/ -mg/ -mg/
< 0.001 mg/ 15.36 mg/ -mg/
<v 0.0002 mg/ 0.04 mg/ 0.035 mg/ ^ » 72 mg/
< 0.001 mg/ 0-40 mg/
< 0.001 mg/ 4 5.0 mg/ 10.0 mg/ 0.003 mg/
Ford Chemical Laboratory, Inc.
36
LABORATORY. INC.
Bacteriological and Chemical Analysis 40 WEST LOUISE AVENUE SALT LAKE CITY, UTAH 84115 PHONE 485-5761
Date:
August 17, 1976
Onmo Utah State University
ATTN: George Hart address Forestry Science Laboratory
CERTIFICATE OF ANALYSIS
76-5007
Logan, Utah 84 321
Iample Water Labeled Gage Received on July 23, 1976, Zion Park Research
urbidity
Conductivity
>H
otal Dissolved Solids it 180° C.
alkalinity as CaCOs
aluminum as Al
trsenic as As
icarbonate as HCOs
arium as Ba
oron as B
ladmium as Cd
!alcium as Ca
arbonate as CO3
hloride as CI
ihromium as Cr (Hex)
yanide as Cn
opper as Cu
20.0
JTU
820.0 umhos/cm
7.56
535.0
234.0
-mg/ _mg/
0.070 mg/
0.008 mg/
2 02.5 mg/
0.144 mg/
<0.001 mg/
CO. 001 mg/
51. 2 mg/
^0.01
90.0
mg/
mg/
^0.001 mg/
<Q.Q1 mg/
0-006 mg/
Fluoride as F
Total Hardness as CaCOs
Iron (Total) as Fe
Iron (Filtered) as Fe
Lead as Pb
Magnesium as Mg
Manganese as Mn
Mercury as Hg
Nitrate as NO,-N
Phosphate as PO4
Potassium as K
Selenium as Se
Silica as SiCX
Silver as Ag
Sulfate as SO*
Sodium as Na
Zinc as Zn
0.32 mg/
234.0 mg/
0.120 mg/
0.100 mg/
O-005 mg/
25.4 mg/
0-035 mg/
^0.0002 mg/
0.02
-m9/ 0.065 mg/ 3.32 mg /
0-077 mg/
9.9
— mg/
<C 0.001 mg/
92.0 mg/
73.0 mg/
0.007
-mg/
Ford Chemical Laboratory, Inc.
37
LABORATORY, INC.
Bacteriological and Chemical Analysis 40 WEST LOUISE AVENUE SALT LAKE CITY, UTAH 84115 PHONE 485-5761
Date:
June 6, 1977
Name Utah State University Forest Department
Address ATTN : Mr ♦ George Hart 860 North 12th East
Logan, UT 84321
CERTIFICATE OF ANALYSIS
77-2632
c , Water Labeled NFl/R at Gage Received on May 16 , 1977: oample _
Turbidity Conductivity
PH
Total Dissolved Solids at 180° C.
Alkalinity as CaCOs
Aluminum as Al
Arsenic as As
Bicarbonate as HCO3
Barium as Ba
Boron as B
Cadmium as Cd
Calcium as Ca
Carbonate as CO3
Chloride as CI
Chromium as Cr (Hex)
Cyanide as Cn
Copper as Cu
2.00
900.0
7.81
600.0
168.0
0.071
< 0.001
204.9 0.091
0.22
130.0
< 0.001
<. 0.01
0.007
JTU
-umhos/cm
_mg/ _mg/ _mg/ _mg/ _mg/ __ mg/ mg/
< 0.001 mg/
21» 6 mg/
<0-01 mg/
_ mg/
-mg/ .mg/
-mg/
Fluoride as F
Total Hardness as CaCOs
Iron (Total) as Fe
Iron (Filtered) as Fe
Lead as Pb
Magnesium as Mg
Manganese as Mn
Mercury as Hg
Nitrate as NO,— N
Phosphate as PO«
Potassium as K
Selenium as Se
Silica as SiCX
Silver as Ag
Sulfate as SO*
Sodium as Na
Zinc as Zn
0.28
230.0
0.086
0.050
-C 0.001
42.24
0.034
< 0.0002
0.10
0.035
A 0.001
82.0
0.042
-mg/
-mg/1
-mg/1
-mg/1
-mg/1
-mg/1
-mg/1
-mg/1
-mg/1 -mg/1
3.14
mg/
< 0.001 mri/1
^ mg/i
21.5 „ mg/1
-mg/1
-mg/'
-mg/1 -mg/1
122.50
Ford Chemical Laboratory, Inc.
38
LABORATORY, INC.
Bacteriological and Chemical Analysis 40 WEST LOUISE AVENUE SALT LAKE CITY, UTAH 84115 PHONE 485-5761
Date:
June 6, 1977
Name
Utah State University Forest Department
»,, ATTN: Mr. George Hart
s 86U North 12th East
Logan, UT 84321
CERTIFICATE OF ANALYSIS
77-2633
Sample Water Labeled East Fork Virgin River at Confluence w/VR Dated May 13, 1977 Received on May 16, 1977:
Turbidity Conductivity
PH
Total Dissolved Solids at 180° C.
Alkalinity as CaCOs
Aluminum as Al
Arsenic as As
Bicarbonate as HCO3
Barium as Ba
Boron as B
Cadmium as Cd
Calcium as Ca
Carbonate as COs
Chloride as CI
Chromium as Cr (Hex)
Cyanide as Cn
Copper as Cu
2.50
600.0
7.73
150.0
0.025
< 0.001
< 0.001
28.0
<
0.003
JTU
.umhos/cm
400.0
_ mg/
_mg/
— mg/ __ mg/ 18 3.0 mg/
0-038 mg/
°'14 _mg/
_ mg/ — mg/
< Q.Q1 mg/
24.0 mg/
0.001 mg/
< 0-01 mg/
-mg/
Fluoride as F
Total Hardness as CaCOs
Iron (Total) as Fe
Iron (Filtered) as Fe
Lead as Pb
Magnesium as Mg
Manganese as Mn
Mercury as Hg
Nitrate as NO.-N
Phosphate as PO<
Potassium as K
Selenium as Se
Silica as Si02
Silver as Ag
Sulfate as SO<
Sodium as Na
Zinc as Zn
0.35
< 0.001
36.0
0.009
< 0.0002
0.70
0.045
< 0.001
22.0
< 0.001
97.0
-mg/
2 2 0.0 mg/
0-079 mg/
°'050 mg/
.mg/
-mg/ -mg/ -mg/
-mg/
-mg/ 2-9? mg/
-mg/ -mg/ -mg/ -mg/
30.30 mg/
0.02 0 mg/
Ford Chemical Laboratory, Inc.
39
LABORATORY, INC.
Bacteriological and Chemical Analysis 40 WEST LOUISE AVENUE SALT LAKE CITY, UTAH 84115 PHONE 485-5761
Date:
June 6, 1977
Name Utah State University
\6d
Forest Department ress ATTN: Mr. George Hart 860 North 12th East Logan, UT 84321
>ample
CERTIFICATE OF ANALYSIS
77-2634
Water Labeled LaVerkin Creek at Hurricane Received on May 16, 1977
'urbidity
lonductivity
>H
"otal Dissolved Solids it 180° C.
Alkalinity as CaCOs
Aluminum as Al
Arsenic as As
licarbonate as HCO3
barium as Ba
boron as B
admium as Cd
alcium as Ca
arbonate as CO3
hloride as CI
hromium as Cr (Hex)
yanide as Cn
opper as Cu
3.00
7.62
180.0
0.043
<0.001
219.6
0.048
0.22
< 0.001
86.4
< 0.01
16.0
< 0.001
< 0.01
0.005
JTU
1/670.0 umhoS/cm
1,105.0
_mg/
-mg/ _mg/ -mg/ -mg/ -mg/ -mg/ -mg/
-mg/ -mg/ -mg/ -mg/ -mg/ -mg/
Fluoride as F
Total Hardness as CaCOa
Iron (Total) as Fe
Iron (Filtered) as Fe
Lead as Pb
Magnesium as Mg
Manganese as Mn
Mercury as Hg
Nitrate as NO ~N
Phosphate as PO4
Potassium as K
Selenium as Se
Silica as Si02
Silver as Ag
Sulfate as SO*
Sodium as Na
Zinc as Zn
<^
0.40
486.0
0.096
0.044
< 0.001
64.8
0.027
-mg/ -mg7 -mg/1
-mg/1 -mg/1
-mg, -mg/1
<, 0.0002 mg/1
_._9^.3 6 mg
0-045 mq/1
2.93 mg/1
<_oJLooi__mg/1
26 . 0 mg/l
0.005 mg/1
58 0.0 mg/1
14 3.0 mg/1
0.025 mg/1
£.
Ford Chemical Laboratory, Inc.
40
LABORATORY, INC.
Hacteriotngical and Chemical Analysis 40 WEST LOUISE AVENUE SALT LAKE CITY, UTAH 84115 PHONE 485 5761
Date:
August 23, 1977
\AQme Utah State University Department ot Forestry
i , . UMC 52
S ATTN: Mr. George Hart Logan, UT 84321
CERTIFICATE OF ANALYSIS 77-4237
ample
Wa
ter Labeled East Fork Virgin River at North Fork Conf.; Received on
August 5, 1977:
urbidity
Conductivity
iH
otal Dissolved Solids t 180° C.
Jkalinity as CaCOs
Juminum as Al
.rsenic as As
icarbonate as HCOs
arium as Ba
oron as B
admium as Cd
alcium as Ca
arbonate as CO3
hloride as CI
hromium as Cr (Hex)
yanide as Cn
opper as Cu
1.6
JTU
490.0
.umhos/cm
8.10
316.0
148.0 0.113
_mg/l
mg/1
mg/1
^°-001 mg/1
180-6 mg/1
0.04 0 mg/1
°'17 _mg/l
_mg/l
55. 2 mg/1
< 0.001
<y 0.01
-mg/1
24.0 mg/1
^0.001 mg/i
•^ n.01 mg/1
0.002
Fluoride as F
Total Hardness as CaCOs
Iron (Total) as Fe
Iron (Filtered) as Fe
Lead as Pb
Magnesium as Mg
Manganese as Mn
Mercury as Hg
Nitrate as NCX-N
Phosphate as PO4
Potassium as K
Selenium as Se
Silica as Si02
Silver as Ag
Sulfate as SO*
Sodium as Na
Zinc as Zn
0.17
-mg/
.mg/ _mg/ -mg/
<_qJLooi_ _mg/
22 -08 mg/
-mg/ -mg/
230.0
0.125 0.100
< 0.0002
0.70
0.010
3.57
0.003
8.0
< 0.001
98.0
24.38
0.008
-mg/1
-mg/ -mg/ -mg/ -mg/ -mg/ -mg/ -mg/ -mg/ -mg/
uports on- submitted Oi th<- confidential property ot dienl Aullun/ution t^< puLI >ur written approval 01 o mutual protection to clients, ttie public und ourselves.
/ .
Ford Chemical Laboratory, Inc.
I our reports, conclusions, or i-xtruets Irani uf regarding iln-ni, is rubc-rved pend /
vt&lsJum/xwl
LABORATORY, INC.
Bacteriological and Chemical Analysis 40 WEST LOUISE AVENUE SALT LAKE CITY, UTAH 84115 PHONE 485 5761
41
Date:
August 23, 1977
MnrnA Utah State University Department of Forestry
Mdress °£"
ATTN: Mr. George Hart
Logan, UT 84321
CERTIFICATE OF ANALYSIS 77-4238
>ample Water Labeled Laverkin Creek at Lees Pas3 Trail Bacaisaad nn August 5, 1977:
"urbidity
Conductivity
to
'otal Dissolved Solids it 180° C.
alkalinity as CaCOs
aluminum as Al
Arsenic as As
bicarbonate as HCOs
iarium as Ba
•oron as B
admium as Cd
alcium as Ca
arbonate as COs
hloride as CI
hromium as Cr (Hex)
yanide as Cn
opper as Cu
1.5
7.97
432.0
148.0
0.063
•< 0.001
180.6
0.063
0.15
< 0.001
84.8
-C
8.0
n.noi
o.oi
0.002
JTU
677 f,0 u m h os/c m
_mg/
_mg/ _mg/ _mg/ _mg/ _mg/ _mg/ _mg/ _mg/ * °-°l __mg/ _mg/
-mg/ .mg/
-mg/
Fluoride as F
Total Hardness as CaCOs
Iron (Total) as Fe
Iron (Filtered) as Fe
Lead as Pb
Magnesium as Mg
Manganese as Mn
Mercury as Hg
Nitrate as N03-N
Phosphate as P04
Potassium as K
Selenium as Se
Silica as SiOz
Silver as Ag
Sulfate as SO<
Sodium as Na
Zinc as Zn
0.20
330.0
0.069
0.040
-^ 0.001
2.3293
.mg/ -mg/ -mg/ -mg/ -mg/ -mg/ -mg/ <. 0.0002 mg/
0-010 mg/
0-010 mg/
2.653
, mg/
< 0.001
0.004
7.0
0.014
— mg/ — mg/ — mg/ — mg/ 17.10 mg/
— mg/
202.0
0.006
/
L-poru an.- submitted oi ihw confidential properly i ilii-nl Author i/olion lor pulili >ur written uppr.i.al a> a mutual protection ro client*, Ihu public und ourselves,
Ford Chemical Laboratory, Inc.
i our r. purls, conclusion., cr. iv trocls Irani or regarding them, is reserved pend ,
/ /
42
LABORATORY, INC.
Bacteriological and Chemical Analysts 40 WEST LOUISE AVENUE SALT LAKE CITY, UTAH 84115 PHONE 485 5761
Date:
September 26, 1977
NJnmg Utah State University Department of Forestry
\ddress ATTN; Mr. George Hart UMC 52 Logan, UT 84321
CERTIFICATE OF ANALYSIS
77-5017
Sample Water Labeled "La Verkin Creek at Lee Pass Trail" Dated September 4, 1977; Received on September 6, 1977:
'urbidity
Conductivity
>H
otal Dissolved Solids it 180° C.
alkalinity as CaCOs
aluminum as Al
Arsenic as As
•icarbonate as HCOs
iarium as Ba
>oron as B
adrnium as Cd
alcium as Ca
arbonate as COs
hloride as CI
hromium as Cr (Hex)
yanide as Cn
opper as Cu
2.0
655.0
7.80
422.0
152.0
0.149
<0.001
185.4
0.184
0.04
-<0.001
80.8
^0.01
10.0
<0.001
-0.01
0.004
JTU
.umhos/cm
_mg/ _mg/ _mg/ -mg/ -mg/ .mg/ _mg/ -mg/
-mg/
.mg/ -mg/ -mg/ -mg/ -mg/
Fluoride as F
Total Hardness as CaCOs
Iron (Total) as Fe
Iron (Filtered) as Fe
Lead as Pb
Magnesium as Mg
Manganese as Mn
Mercury as Hg
Nitrate as NO,— N
Phosphate as PO<
Potassium as K
Selenium as Se
Silica as Si02
Silver as Ag
Sulfate as SO*
Sodium as Na
Zinc as Zn
0.15
336.0
0.133
0.100
0.001
32.16
0.007
A 0.0002
<0.01
0.01
3.70
0.001
8.0
S 0.001
194.0
11.93
0.033
Ford Chemical Laboratory, Inc.
-mg/ -mg/ -mg/ -mg/ _mg/ -mg/ -mg/ -mg/ -mg/ -mg/ -mg/ -mg/ -mg/ -mg/ -mg/ .mg/ .mg/
eporis ore submitted as the confidential property of clients Authorization for publ cjtioii of our reports, conclusions, or, extracts from or regarding them, is reserved pend- )ur written approval as a mutual protection to clients, the public and ourselves.