Angela's Tools · Chapter 18 · The Water Cycle Lab 3 of 3 · Recording sheet

Roll the Dice: Where Does a Water Molecule Go, and How Long Does It Stay?

Investigation question: If you follow one water molecule through a chance-based model of the water cycle, where does it spend most of its time, which processes move it, and how well does the model match Earth's real reservoirs?

Collaborative systems modelingGroups of 31 session Setup 8 · Activity 42 · Cleanup 5 min MS-ESS2-4 · assesses
NameGroupDate

Your role today

Safety

Procedure

  1. Before moving, write your prediction in q1: at which station will your molecule spend the most rolls, and which processes will move it most often? Give a reason.
  2. Go to your assigned starting station. Record it as move 0 in the journey log and, if using beads, thread one bead of that station's color.
  3. On the teacher's signal, the Traveler rolls the die once. The Process checker reads the rule for that number on the station sign and says the process and the driver aloud. The Recorder writes the move: station, roll, 'stayed' or the new station, the process, and the driver (Sun, gravity, cooling, or 'held' for a stay).
  4. If the rule says move, walk to the new station and thread a bead of its color; if it says stay, thread another bead of the same color and wait for the next signal. Keep going for 15 moves.
  5. After the last move, complete the group tally: for each station, count how many rolls you made there and how many of those were stays. Count the processes by driver.
  6. Add your group's numbers to the class tally chart. When all groups are in, compute for each station: departures = total rolls minus stays, and average stay = total rolls ÷ departures (if a station has zero departures, write 'no departures').
  7. Draw your route as a network on the recording sheet: a circle for each station you visited, an arrow for each move, labeled with the process, with loops for stays.
  8. Compare the class's average-stay ranking to the approximate real residence-time table, and answer the analysis questions individually.
  9. If time allows, each group proposes one rule change for one station that models a real scenario (a warm winter with rain instead of snow, a drought, heavy pumping of groundwater, a paved city) and predicts how the class data would change. Play 8 more moves with the changed rule at that station and check the prediction.

Record your observations

Lab 3 recording sheet: Roll the dice through the water cycle

The station rules below are also posted on the station signs. The die decides every move; your job is to record it accurately, name the process and its driver, and then analyze the class's pooled data.

Station rules (roll a six-sided die)
StationRolls 1-2Rolls 3-4Roll 5Roll 6
OceanStay: carried by currentsStay: carried by currentsEvaporation to Atmosphere (Sun)Evaporation to Atmosphere (Sun)
AtmosphereCondensation, then rain to Ocean (cooling, then gravity)Rain to River (roll 3) or to Soil (roll 4) (cooling, then gravity)Snow to Snowpack (cooling, then gravity)Rain to Lake (cooling, then gravity)
Snowpack and glacierStay: frozen in placeStay (roll 3) or melting to River (roll 4) (Sun, then gravity)Melting, then infiltration to Soil (Sun, then gravity)Sublimation to Atmosphere (Sun)
RiverStay (roll 1) or flow to Ocean (roll 2) (gravity)Flow to Ocean (roll 3) or to Lake (roll 4) (gravity)Evaporation to Atmosphere (Sun)Seep through the riverbed to Groundwater (gravity)
LakeStay: held in the lakeStay (roll 3) or outflow to River (roll 4) (gravity)Evaporation to Atmosphere (Sun)Seep to Groundwater (gravity)
SoilStay (roll 1) or evaporation to Atmosphere (roll 2) (Sun)Root uptake to Plant (Sun, via transpiration pull)Infiltration to Groundwater (gravity)Runoff to River (gravity)
PlantStay (roll 1) or transpiration to Atmosphere (roll 2) (Sun)Transpiration to Atmosphere (Sun)Transpiration to Atmosphere (Sun)Transpiration to Atmosphere (Sun)
GroundwaterStay: creeping through poresStay: creeping through poresSpring flow to River (gravity)Seep out under the sea to Ocean (gravity)
1.Prediction: at which station will your molecule spend the most rolls, and which driver (Sun, gravity or cooling) will move it most often? Explain using the rules.
Journey log
MoveStationRollStayed, or moved toProcessDriver (Sun / gravity / cooling / held)
0 (start)
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
Group tally
StationRolls we made hereOf those, staysMoves driven by the SunMoves driven by gravityMoves that began with cooling
Ocean
Atmosphere
Snowpack and glacier
River
Lake
Soil
Plant
Groundwater
Class tally (copy from the board)
StationTotal rolls (all groups)StaysDepartures (rolls minus stays)Average stay (rolls ÷ departures)Rank (1 = longest stay)
Ocean
Atmosphere
Snowpack and glacier
River
Lake
Soil
Plant
Groundwater
Approximate real residence times (rough estimates; sources differ)
ReservoirTypical time water stays
Oceanthousands of years
Groundwateryears to thousands of years
Glaciers and ice sheetsdecades to many thousands of years
Lakesyears to centuries
Seasonal snowpackmonths
Soil moistureweeks to months
Riversweeks to months
Plantsdays
Atmosphereabout 9 days
✎Draw your route as a network: a circle for each station you visited, one arrow per move labeled with its process, and a loop on a circle for each stay. Mark Sun-driven arrows with a small sun and gravity-driven arrows with a down arrow.
2.After 15 moves: how many different stations did you visit, where was your longest stay and how long was it, and did your prediction in q1 hold? Explain.

Analysis questions

3.Using the class tally, calculate the average stay for the Ocean and for the Atmosphere (average stay = total rolls ÷ departures). Show the numbers. Then explain, using the station rules, why these two values are so different.
4.Compare the class's average-stay ranking with the approximate real residence-time table. Name two reservoirs where the model's ranking agrees with reality and one where it does not, and explain what a single roll stands for in each case.
5.From your group tally, which driver moved your molecule most often: the Sun, gravity or cooling? Explain why every move out of the Atmosphere counts as 'cooling, then gravity' and why no move out of the Ocean counts as gravity.
6.Find a stretch of your route that never touched the Ocean, or one that went up and down between the ground and the air more than once. Describe it, name the processes, and explain why Earth's real water cycle allows that route.
7.Propose one rule change for one station that models a real change: a warm winter with rain instead of snow, a long drought, heavy pumping of groundwater for irrigation, or a city paving over its soil. Write the new rule, say which real process it represents, and predict how the class's average stay at two stations would change.
8.List three things about the real water cycle that this dice model cannot show, and for one of them explain how you would change the model to include it.
Angela's Tools · Chapter 18 · The Water CycleLab 3 of 3 · Student recording sheet