Lab / experiment Grade 9 Science

Verrin River Thermal Mixing: Heat, Equilibrium, and Oxygen

A grade 9 lab where students mix warm and cold water to find equilibrium temperature, modeling a power plant's thermal mixing zone and its effect on dissolved oxygen.

Objectives

  1. Students will predict and measure the equilibrium temperature reached when warm and cold water are mixed.
  2. Students will use a weighted average to explain unequal-volume mixing and connect warming to lower 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: thermal energy, equilibrium temperature, weighted average, mixing zone

Teacher overview

When a power plant releases warm cooling water into a cooler river, the two flows mix and settle to an in-between temperature, forming what scientists call a thermal mixing zone. This lab models that process on a small scale: students mix warm and cold water, predict the temperature the mixture will reach, and compare it with the measured result. Because cold water holds more dissolved oxygen than warm water, and most fish need dissolved oxygen above 5 mg/L, the lab ends by connecting the temperature change to the health of a river like the fictional Verrin River.

Answer Key

  1. Answer: The average of the two temperatures. For equal volumes, the predicted mix is (cold temp + warm temp) / 2. Accept any value that matches the average of the student's own two recorded temperatures, reported to about the thermometer's precision. Extra decimal places would claim more accuracy than the thermometer readings have.
  2. Answer: Answers will vary. The measured value is usually slightly below the prediction because some heat is lost to the cup and the surrounding air, so the closed-system ideal is not perfectly met. Accept any answer consistent with the student's data and a valid reason.
  3. Answer: 30 C. With equal volumes, the equilibrium is the simple average: (40 + 20) / 2 = 30 C.
  4. Answer: 35 C. Weighted by volume: (300 x 40 + 100 x 20) / (300 + 100) = (12,000 + 2,000) / 400 = 14,000 / 400 = 35 C. The larger warm volume pulls the mixture closer to 40 C.
  5. Answer: The second law says thermal energy moves from the warmer to the cooler water until the energy is more uniformly distributed, giving one in-between temperature. Accept any answer stating that heat spread until both parts reached the same temperature, matching the single mixed reading observed.
  6. Answer: Accept any answer explaining that adding warm water raises the river's temperature in the mixing zone, and warmer water holds less dissolved oxygen. If the oxygen drops near or below 5 mg/L, fish can be stressed or forced to leave. The lab models this because mixing warm and cold water produced a warmer result than the cold water alone.

Differentiation

Support

Pre-measure the warm and cold water for each group and provide a data table with Trial 1 volumes already filled in, so students focus on reading thermometers and averaging. Give a worked averaging example with different numbers before Step 4.

Extension

Have students test a third trial that predicts, before mixing, the exact volumes of warm and cold water needed to hit a target mixed temperature, then check their prediction by measurement and explain any gap using heat loss.

ELL supports

Provide labeled picture cards for "warm," "cold," and "mix," and a sentence frame for the analysis: "I predicted ___ C and measured ___ C because ___." Allow students to record temperatures in the table before writing full sentences.

Extensions

Have students look up the temperature and dissolved-oxygen readings from a nearby river or lake monitoring station across the seasons, and describe how the summer warming they see in the real data matches the pattern their small mixing experiment demonstrated.