ViewWiki

Lesson 2 of 5

Groundwater and aquifers.

About 35 minutes · 9 practice questions

Under your feet, between the grains of sand, there is water. Use Darcy’s law to work out how slowly it creeps, find how much a well can give before it runs dry, and see what drought and over-pumping do to an aquifer.

Step 1 of 9 · Under the ground

Step 1 of 9

Under the ground

In the last Lesson some of the rain soaked into the ground. In the Scene there is a block of ground: a layer of fine sand, and below it clay that water cannot pass, between two streams 2 km apart. In the middle there is a well with a pump. Cut into the ground has taken away the dry sand back to the plane of the well, and what is left is the part soaked with water. Pumping rate is now zero.

To the question

Step 2 of 9

Rain and the water table

The rain soaking in reaches the water table, and the water flows slowly through the sand from the middle to the streams, which hold the water table at their level. So the water table is not flat: it is a low mound between the two streams, and a stream fed by groundwater keeps flowing even in summer.

To the question

Step 3 of 9

Darcy’s law

How fast does groundwater flow? In 1856 the French engineer Henry Darcy measured water flowing through columns of sand, and found that the flow grows with the hydraulic gradient i=ΔhLi = \dfrac{\Delta h}{L}⁠, how far the water table falls in each metre of the way:

q=K iq = K\,i⁠

KK⁠ is the hydraulic conductivity: many metres a day in gravel, a few metres in fine sand, and almost zero in clay. Rainfall is locked.

To the question

Step 4 of 9

A cone round the well

When the pump runs, it takes water out of the well, and the water in the sand around flows towards it. To flow, the water table must slope down to the well, and so a cone forms round it. The more you pump, the deeper the cone, and the label over the well shows how far the water in it has dropped.

To the question

Step 5 of 9

A drought

Pumping rate is now 400 m³ a day, water for a town, and the well gives all of it.

To the question

Step 6 of 9

Over-pumping

In a drought, and with heavy pumping, the well runs dry and the cone is wide and deep. When more is pumped over time than the rain puts back, the water table falls year after year, and streams and springs fed by the groundwater dry up. Near the sea there is one more consequence.

To the question

Step 7 of 9

A wet year

More rain raises the mound of groundwater, and its slope down to the streams gets steeper.

To the question

Step 8 of 9

Pumping harder

The town grows and needs more water. It pumps more from the same well.

To the question

Step 9 of 9

Above the pump

A pump in a well needs water above it. If the level drops below it, it sucks air.

To the question

Still of the Groundwater and aquifers 3D scene
Interactive scene

Loading the interactive version…

Each step sets up the Scene for you, and a control marked “fixed” stays put for that step.

To the experiment

Practice · Choose

Cut into the ground has taken away the dry sand above the water table. Where exactly is the groundwater?

To the experiment

Practice · Predict, then look

With no pumping, the rain raises the water table into a mound between the two streams. Predict: what will happen to that mound if Rainfall drops from 800 mm a year to a drought of 100 mm?

To the experiment

Practice · Calculate

Rainfall is locked at 800 mm a year, with no pumping. In the middle the water table stands about 6 m above the streams, which are 1000 m away. The fine sand’s hydraulic conductivity is K=2K = 2⁠ metres a day, and its porosity is n=0.3n = 0.3⁠. How long does the water take to creep from the middle to the stream?

To the experiment

Practice · Reach the target

Rainfall is locked at 800 mm a year. Raise Pumping rate to the most the well gives without running dry, to within 12 m³ a day, and press Check.

To the experiment

Practice · Predict, then look

The town pumps 400 m³ a day, and the well gives all of it. Predict: what will happen if Rainfall drops to a drought of 100 mm a year and the town keeps asking for the same?

To the experiment

Practice · Choose

Israel’s Coastal Aquifer meets the Mediterranean. Under the shore, the fresh groundwater floats on salty, heavier sea water. What happened where it was over-pumped for years?

To the experiment

Practice · Calculate

Rainfall is locked at 1600 mm a year, a very wet year, with no pumping. In the middle the water table stands 10.8 m above the streams, which are 1000 m away. What is the hydraulic gradient, i=ΔhLi = \dfrac{\Delta h}{L}⁠?

To the experiment

Practice · Predict, then look

The Pumping rate is 200 m³ a day, and the water in the well has dropped 6.3 m. Predict: by how much will the water in the well drop when the town pumps twice as much, 400 m³ a day?

To the experiment

Practice · Reach the target

Rainfall is locked at 800 mm a year. The pump hangs 15 m above the clay layer. Raise the Pumping rate until exactly 15 m of water stand in the well above the clay, and press Check.