Lab / experiment Grade 10 Science

Why Lakes Warm Slowly: A Water Specific-Heat Mixing Lab

A grade 10 lab where students mix measured hot and cold water, predict the final temperature with a weighted average, and link it to water's high specific heat.

Objectives

  1. Students will predict the final temperature of mixed hot and cold water using a weighted average.
  2. Students will compare measured and predicted final temperatures and account for heat loss.
  3. Students will explain how water's high specific heat moderates lake temperature and dissolved oxygen.

Vocabulary

Dissolved oxygen
Dissolved oxygen is the oxygen gas mixed into water that fish and other underwater animals breathe. Cold, moving water holds more oxygen than warm, still water.

Also: specific heat, thermal energy, weighted average, equilibrium temperature

Teacher overview

Water resists changing temperature because it has a high specific heat, and that property helps explain why a deep lake stays cooler than the air on a hot afternoon. In this lab, students mix measured amounts of hot and cold water in an insulated cup, record the final temperature, and compare it to a prediction from a mass-weighted average. Because both samples are water, the predicted final temperature is simply the weighted average of the two starting temperatures. The classroom setup is a simplified stand-in for a lake, not a precise calorimeter, but it shows the same energy-sharing principle at work.

Answer Key

  1. Answer: 35 degrees C. Predicted final = (100 x 60 + 100 x 10) divided by 200 = (6,000 + 1,000) divided by 200 = 7,000 divided by 200 = 35 degrees Celsius.
  2. Answer: 47.5 degrees C. Predicted final = (150 x 60 + 50 x 10) divided by 200 = (9,000 + 500) divided by 200 = 9,500 divided by 200 = 47.5 degrees Celsius.
  3. Answer: Varies by group's data. The measured value is usually a few degrees lower than the predicted 35 degrees C because some heat escapes to the cup and the air. Accept any answer that correctly states the direction and size of the difference from the student's own data.
  4. Answer: The hot water lost thermal energy and the cold water gained the same amount until both reached one shared temperature. Because both samples are water with the same specific heat, equal masses changed temperature by equal amounts in Trial 1, so the mixture settled near the middle rather than staying hot or cold. Water's high specific heat matters when water exchanges energy with something else, such as air or sunlight, as in question 5.
  5. Answer: A deep lake holds a large mass of water with a high specific heat, so it absorbs a lot of solar energy for only a small temperature rise. That large heat capacity lets the lake warm and cool much more slowly than the air, keeping its temperature steadier through the day.
  6. Answer: Warm water holds less dissolved oxygen, so as a shallow pond heats up its oxygen drops. If it falls below the 5 mg/L that most fish need, the fish can suffocate, which is why fast summer warming in shallow water threatens fish.

Differentiation

Support

Pre-fill the starting temperatures (60 and 10 degrees C) on the data table and work Trial 1's predicted value with the class before groups run their own trials. Provide the weighted-average formula with each term labeled.

Extension

Have students design a third trial that predicts a final temperature of exactly 25 degrees C using the same 60-degree and 10-degree water, solve for the volumes needed, then test their prediction and explain any difference from the measured result.

ELL supports

Pair "specific heat," "thermal energy," and "equilibrium temperature" with simple pictures of a hot cup and a cold cup combining into one warm cup. Allow students to record measurements as numbers in the table and to answer questions 4 through 6 with a labeled sketch plus a short phrase.