It's Raining, It's Pouring: Chemical Analysis of Rainwater

Objective

The goal of this project is to assess the water quality of rainwater collected from different geographical areas. The water quality measures used in this project are hardness, pH, and plant growth. Additional measures could be chosen to expand this project.

Introduction

Is the chemistry of rainwater from different geographical regions similar or different? How does rainwater chemistry relate to that of local surface water? How is rainwater chemistry affected by large-scale weather patterns? Does rainwater chemistry affect the growth of plants? These are some of the many questions you could choose to pursue with this project.

This project is based on Jonathan Allison's 2003 California State Science Fair entry. Here is how Jonathan summarized his experimental procedure: "I contacted friends and family from 11 different cities in the United States and asked them if they could help me by collecting rainwater from their city. After they collected it, they shipped it back to me. Then I tested the rainwater for hardness, using the chemical process of titration. Next I tested the rainwater for pH levels. Then I planted radish seeds in potting soil and watered each set of seedlings with rainwater from a different city. I observed, measured and recorded any growth or changes daily for seven days." (Allison, 2003)

Water Hardness

Water hardness is a measure of dissolved compounds (e.g., magnesium carbonate, calcium carbonate) in the water. These compounds can precipitate out in boilers and water heaters (scaling). Hard water makes less suds with soap and detergent, so you need to use more soap and detergent to get clothes and dishes clean with hard water. General guidelines for classification of waters are: 0 to 60 mg/L (milligrams per liter) as calcium carbonate is classified as soft; 61 to 120 mg/L as moderately hard; 121 to 180 mg/L as hard; and more than 180 mg/L as very hard (USGS, date unknown).

Figures 1 and 2 show USGS water hardness data for the continental United States. Figure 1 is a histogram showing the mean hardness data for each of the 344 stations sampled. Figure 2 is a map of the U.S., showing the regional patterns of groundwater hardness. In both cases, the data is from 1975, but the patterns shown have proven to be stable over time.

Histogram of U.S. groundwater hardness from 344 collection stations.
Figure 1. Histogram of U.S. groundwater hardness from 344 collection stations (USGS, 1975 data).

Map of U.S. groundwater hardness from 344 collection stations.
Figure 2. Map of U.S. groundwater hardness from 344 collection stations (USGS, 1975 data).

pH

Acidity and alkalinity are measured with a logarithmic scale called pH. pH is the negative logarithm of the hydrogen ion concentration:

pH = −log [H+] .

What this equation means is for each 1-unit change in pH, the hydrogen ion concentration changes ten-fold. Pure water has a neutral pH of 7. pH values lower than 7 are acidic, and pH values higher than 7 are alkaline (basic). The table below has examples of substances with different pH values (Decelles, 2002; Environment Canada, 2002; EPA, date unknown).

Table 1. The pH Scale: Some Examples
pH ValueH+ Concentration
Relative to Pure Water
Example
010 000 000battery acid
11 000 000sulfuric acid
2100 000lemon juice, vinegar
310 000orange juice, soda
41 000tomato juice, acid rain
5100black coffee, bananas
610urine, milk
71pure water
80.1sea water, eggs
90.01baking soda
100.001Great Salt Lake, milk of magnesia
110.000 1ammonia solution
120.000 01soapy water
130.000 001bleach, oven cleaner
140.000 000 1liquid drain cleaner

Figure 3 shows a map of the average pH of precipitation in the continental U.S. for the year 1992. "The areas of greatest acidity (lowest pH values) are located in the Northeastern United States. This pattern of high acidity is caused by the large number of cities, the dense population, and the concentration of power and industrial plants in the Northeast. In addition, the prevailing wind direction brings storms and pollution to the Northeast from the Midwest, and dust from the soil and rocks in the Northeastern United States is less likely to neutralize acidity in the rain." (USGS, 1997)

Map of U.S. annual average precipitation pH (1992 data).
Figure 3. Map of U.S. annual average precipitation pH for 1992. (USGS, 1997).

Plant Growth

Most plants prefer soil that is near neutral pH. There are particular varieties (strawberries, azaleas and rhododendrons, for example) that prefer acidic soil. Soil pH also influences how readily available many soil nutrients are to plants.

Terms, Concepts and Questions to Start Background Research

To do this project, you should do research that enables you to understand the following terms and concepts:

  • titration,
  • water hardness,
  • pH.

More advanced students will also want to understand the following terms and concepts:

  • molarity,
  • stoichiometry.

Bibliography

Materials and Equipment

  • This project requires planning ahead. Remember that it will take some time for your volunteers to collect samples and send them to you. You also need to allow time (at least one week) for the plant growth experiment once you have received all of the samples. Start early and make sure your volunteers send their samples in a timely manner!
    • Where to get samples? You will need to obtain rainwater samples from a wide geographical area. Consult the maps in the Introduction for historical patterns of variation. Ask friends and relatives to collect samples for you.
    • How much water do I need? Check your test kit instructions (see below) to see how much water is required for each test (usually about 5 ml). You will want to repeat your tests for each sample at least 3 times to assure that your results are consistent. So you'll need a minimum of 30 ml just for testing (best to plan on more). You will also need water for the plant growth experiment. Calculate how much water you will need for plant growth, and add 50 ml for testing purposes. This is how much rainwater each of your volunteers will have to send to you.
    • How should my volunteers collect rainwater samples? Simply putting a jar out on the lawn during a rainstorm is not going to be very efficient. In order to get enough water, your volunteers need a large catchment area. Probably the most straightforward solution is to collect water from the roof, by placing a collection jar underneath a downspout.
    • Make sure your volunteers label the water sample with the date and location from which it was collected.
  • For performing the water quality tests, the simplest method is to use a pre-packaged kit designed for testing aquarium water. There are several different brands available. You should be able to find a choice at a local pet store that sells fish. The kit will say how many water samples it will test. You should be able to find kits to test 50 samples for under $10. The kits you need for this project are:
    • general hardness (GH) test kit,
    • pH test kit.
  • For the plant growth experiment, you'll need:
    • radish seeds, (or other suitable, fast-growing seeds),
    • small containers (peat pots or seedling trays),
    • potting soil, and
    • a measuring device for dispensing water.

Experimental Procedure

  1. For the water hardness and pH tests, follow the instructions that come with the water test kit. When titrating samples, it is important to mix the solution well after each drop of test solution is added.
  2. For the plant growth portion of the experiment, it is important to keep all of the other growth conditions (sun exposure, soil, temperature, etc.) constant, and to vary only the source of water used for the plants. Be sure to use the same amount of water. Consult the Science Buddies resource, Measuring Plant Growth for methods you can use to quantify differences in growth.

Variations

  • Does rainwater chemistry in your area vary with weather patterns? Collect samples over several weeks or months, and test the water quality. Keep track of the weather systems that produced the precipitation. Were there variations in the ultimate source of the moisture? Can you correlate these variations with changes in rainwater chemistry?
  • If you live in an urban area, is rainwater chemistry affected by smog? Check the air quality reported in the newspaper for the days that samples were collected. Do you see differences in rainwater chemistry after days with high smog compared to days with cleaner air?
  • For the samples in your study, how does rainwater hardness compare with groundwater hardness? (See Figure 2 in the Introduction, above.) How does the acidity compare to the 1992 U.S. data? (See Figure 3 in the Introduction, above.)
  • Here are two related Science Buddies projects you might want to check out:

Credits

Andrew Olson, Ph.D., Science Buddies

Sources

This project was based on:

Related Posts by Categories



0 comments:

Engineering News

Central Board of Secondary Education

Architecture News

Management News

Medical News

Journalism News

ss_blog_claim=39d0fbd9150037431cf33bbbf3c7c7ce