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6-10-08
Chase Lake Formal Lab Soil pH
Question: Does the distance from the lake effect the pH of the soil?
Hypothesis: Since Chase Lake is very polluted, I think the lake and the soil closest to the
lake will be more acidic than soil farther inland. If the lake is very acidic it will most likely
leak some of its acidity into the nearest soil, lowering the pH of soil close to the lake incomparison with soil farther away. Also, Chase Lake has probably accumulated a lot of
acidic rain over the years, which should again make the soil closer to the lake have a lower
pH and soil farther away have a higher pH.
Independent Variable: the distance from the lake the soil sample is taken from
Dependent Variable: the pH of the soil sample
Controlled Variables: amount of soil taken, amount of distilled water added to soil, ground
level the soil is taken from, and type of distilled water used to add to the soil and clean theinstruments
Materials:
Small shovel
Plastic 100ml tube with a top cover
Field study tape measure
4 bottles of the same distilled water
pH probe with GLX attachment
access to a lake
Procedure:
1. Use the field tape measure to make a transect extending 2 meters from the edge ofthe lake inland.
2. Fill the tube with 30ml of lake water taken from the area of water adjacent to the
transect.3. Use the pH probe to find the pH of the water and record this data.
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4. Clean off the pH probe with some of the distilled water so its pH returns to normal.
5. Clean out the tube that held the lake water with some distilled water.
6. Measure 40cm away from the waters edge along the transect and use the shovel totake a sample of soil from the grounds surface.
7. Use the soil from the sample and fill the tube with 10ml of soil making sure to pack
the soil down well and evenly with your fingers.8. Fill the tube with an additional 20ml of distilled water so that the overall waterline
in the tube is at 30ml.
9. Close the tube tightly with the cap.10. Shake the tube up so that all the soil is evenly mixed with the water and there are no
major clumps of soil.
11. Open the tube and measure the pH of the soil solution with the pH probe. Record
this measurement.12. Clean out the tube and wash the pH probe with the distilled water.
13. Repeat steps 6-12 except measure 80-cm, then 120cm, then 160cm and finally
200cm from the waters edge so that there is a total of 4 measurements recorded
(including the waters pH).14. Repeat steps 1-13 four more times except make four new, different transects from
as many different regions of the lake as possible.
Data Collection & Processing
Data Table of Soil pH at Chase Lake at Different Transects
Transect Distance from Water (cm) 0.5cm pH of soil 0.1pH
#1 0 (the actual water)
40
80
120160
200
7.05
6.6
6.6
5.45.6
6.1
#2 0 (the actual water)
40
80120
160
200
7.1
6.1
6.15.9
5.9
5.7
#3 0 (the actual water)
40
80120
160200
6.0
5.3
5.66.7
6.55.4
#4 0 (the actual water)
4080
120
6.0
5.35.5
6.1
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160
200
6.3
6.3
Data Table of Average Soil pH out of the 4 Transects
Distance from Water (cm) 0.5cm Average pH of Soil 0.1pH
0 (the actual water itself) 6.540 5.8
80 6.0
120 6.0
160 6.1
200 5.9
Conclusion & Evaluation
According to the average data of soil pH vs. the distance away from the lake taken
from 4 different transects the hypothesis that soil pH will be lower closer to the lake and
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higher farther away from the lake was found to be incorrect. In fact, it seems like
according to the data there is no relationship between soil pH and the distance of the soil
away from the water. From 40cm away to 160cm away the pH seemed to be increasingslightly because the pH values went from 5.8 to 6.1, which isnt too much of a difference
(only 0.3pH), but from 160cm to 200cm the trend ended and the pH decreased from 6.1 to
5.9.In the individual transects there seemed to be no trend in the data either. Distance fromthe water had no bearing on soil pH. For example, in transect #4 the pH increased over
40cm to 200cm from 5.3 to 6.3, but in transect #2 the pH decreased over 40cm to 200cm
from 6.1 to 5.7. Also, the data of the average soil pHs (not including the pH of the wateritself) only fluctuated by about 0.3 pH over the 2 meters, which is not a very significant
difference.
The fact that there was no relationship found between the distance from the waters
edge and soil pH couldve been due to the many sources of error during this experiment.One of the largest sources of error that I saw was the effectiveness of the pH probes.
Despite the fact that we tried to keep the starting pH of the probe constant by always
cleaning it off with water in between measurement sometimes the PH probe would
randomly stay at a low pH of like 6 or a high ph of 8 after having been cleaned and juststanding in the open air. I think that sometimes the pH probes readings were randomly
off. Another source of error was the small sample size of the experiment. We only tookfour transects when we should have tried to do more like ten. If we had done more
transects this wouldve reduced the error caused by problems like when the pH probes
decided not to work right. Another source of error is that there was no way to regulate thematerials incorporated into the soil when the soil sample was taken. For instance, some of
the soil samples taken farther inland had to be dug up from mossy grass whereas the soil
samples taken closer to the water were taken from bare dirt. The soil taken from the grass
might have included plants that were not apart of the soil like moss or grass that could haveeffected the soil pH somehow.
One possible way to improve this lab would be to make the transects longer like 10
meters long, and to still take soil samples every 40cm. By only using 2 meter transects wemight have not noticed trends that continued and took shape later on, farther away from the
lake. Another possible way to improve this lab would be to have taken soil samples right at
the edge of the lake soil samples from the actual lake bed by taking soil from the lake andletting it dry out in a strainer over night and then measuring its pH as we did with the rest
of the soil samples. These extra samples would give us more valuable information like if
there was a difference of soil pH in soil that had been in direct contact with the lake versus
soil samples taken inland. The last way to improve this lab would be to make sure that atransect was taken in every different soil environment from around the lake. For instance,
if there was a part of the lake bordered by trees we shouldve taken a transect there, and if
there was a part bordered by rushes and cattails we should have taken one there andetcetera, etcetera until every different type of land bordering the lake had a transect taken
by it. This would account for any differences in soil pH caused by the vegetation
surrounding the soil, and hopefully minimize the effects of these differences by havingthem all equally represented.