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== Draining an aquifer ==
 
== Draining an aquifer ==
 
Before we will have a look at the double-slit method itself, it is good to know these basic things about the aquifers and how to drain them.
 
  
 
Aquifers produce infinite amounts of water, but they can also absorb infinite amounts of it. We can drain an aquifer into itself either within one z-level or across multiple z-levels.  
 
Aquifers produce infinite amounts of water, but they can also absorb infinite amounts of it. We can drain an aquifer into itself either within one z-level or across multiple z-levels.  
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=== Draining across multiple z-levels ===
 
=== Draining across multiple z-levels ===
  
QuantumMenace's double slit method uses this kind of aquifer draining for all but the lowest aquifer level. Once one of the lower aquifer levels has been cracked open, it can absorb all of the water being produced by the aquifer level above it.  
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QuantumMenace's double slit method uses this kind of aquifer draining for all but the lowest aquifer level. It is more convenient to use the lower aquifer level to absorb all of the water being produced by the aquifer level above it.  
  
 
{|class="wikitable1"
 
{|class="wikitable1"
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| [[Image:Aquifer draining.png|left|350px|]]
 
| [[Image:Aquifer draining.png|left|350px|]]
 
|}
 
|}
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This only works if you crack open the lower aquifer level. You can achieve this by digging stairs or channeling into the lower aquifer level while the upper aquifer level is being pumped dry. After that, the lower aquifer level will be able to receive any water from above.
  
 
=== Drain within one z-level ===
 
=== Drain within one z-level ===
  
The double-slit method uses this for the lowest aquifer level. Here we pump out the water from a tile being flooded by the aquifer to the level above it (which is already secured) and let it flow back down to another tile where it becomes absorbed by the same aquifer layer again. Note that the target tile of the aquifer must be cracked open (e.g. by downstairs or a channel) to be able to receive water.
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The double-slit method uses this for the lowest aquifer level. Here we pump out the water from a tile being flooded by the aquifer to the level above it and let it flow back down to another tile where it becomes absorbed by the same aquifer layer again. Note that the target tile of the aquifer must be cracked open (e.g. by downstairs or a channel) to be able to receive water.
  
 
{|class="wikitable1" style="padding-top: 2em"
 
{|class="wikitable1" style="padding-top: 2em"
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| [[Image:Aquifer_pump_scheme.png|left|600px|Water flow between the two slits.]]
 
| [[Image:Aquifer_pump_scheme.png|left|600px|Water flow between the two slits.]]
 
|}
 
|}
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== Tutorial embark setup ==
 
== Tutorial embark setup ==

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