**Is John Stealing Water?? **John Casey has a cattle ranch near Adin, where he grows pasture and hay to raise about 70 Angus steers. His place is 240 acres with lower irrigated land and forest on the higher part. He has an adjudicated water right of 2.00 cubic feet per second (cfs) from Preacher Creek, to irrigate 80 acres.

John’s downstream neighbors claim he steals water. He says he can show that he takes only 2 cfs, or less when the flow drops down in the summer. Can he prove it?

As we can see, he has a square headgate at the head of his ditch. It is 2.0′ wide, and can open up to 1.5′ high. Right now, John says he is diverting 1.05 cfs. His evidence is that his gate is open 0.15′, the water is 0.57′ deep on the upstream side, and the water is 0.20′ deep on the downstream side. Is that enough to check what he says?

The box in which the gate sits has smooth walls, and the gate closes flush with the bottom when John is not diverting. The water continues in a straight path from upstream to downstream. That means the weir has “suppressed” sides.

This is in contrast with, for example, a hole cut in the middle of a 2″ x 12″ weir board. The water on the sides has to make the turn to go straight through, so the hole in the board is an example of a “contracted” orifice.

Let’s look at the tables for orifices in the back of the **Water Measurement Manual**. Table A9-3 is for submerged, suppressed weirs.

We can’t see the downstream side of the weir, but the water is above the bottom of the edge of the gate, so it is submerged rather than free-flowing.

This table has flows calculated for a minimum area of 2.0 square feet (sq. ft.). However, the area of the opening at John’s headgate is 2.0′ wide x 0.15′ high, or 0.30 sq. ft. Fortunately, the equation, Q=0.70A(2g Δh)^0.5, is listed right at the top of the table. We can calculate the flow using that. Q is the flow in cfs, A is the area of the orifice hole, g = the acceleration due to gravity, or 32.2 ft/second^2 (feet per second squared), and Δh is the difference between the upstream and downstream water depth.

So the flow Q = 0.70 x (2.0′ x 0.30′) x (2 x 32.2 x 0.37′)^0.5 = 1.03 cfs. So far so good – John is taking 52%, or just over half of his right when 100 percent of flows are available. But, how much flow is actually available right now?

Let’s use the “**sum of the boxes**” method. Instead of measuring the amount of water in Preacher Creek at the top, before any diversions, and then estimating how much flow is being lost to evaporation, transpiration, and infiltration, and then estimating how much flow is subsurface above John Casey’s ranch and “pops up” out of the ground below, we’ll look at what each diversion amount is, plus the amount still in the creek after the last diversion. This is very useful because none of the instream losses have to be estimated – we just add the diversions and flow still in the creek, and that amount IS the available supply. Some Superior Court judges in past decades were pretty smart and actually ordered that available flows be calculated this way.

*The paragraph above, from the Susan River Decree, defines available water supply as what is being diverted, plus the flow passing the last diversion.*

There are 4 diversions on Preacher Creek, and here are the amounts being diverted:

- Diversion 1 (John Casey) 1.03 cfs of a 1.60 cfs water right, 52% of his total right
- Diversion 2 (Amy Hoss) 1.67 cfs of a 3.80 cfs water right, 44% of her total right
- Diversion 3 (Mark and Cindy Sample) 0.55 cfs of a 0.88 cfs water right, 62% of their total right
- Diversion 4 (Quint and Marcie Minks) 1.32 cfs of a 2.50 cfs water right, 53% of his total right
- Flow still in the creek past the Minks Diverison – Quint estimates about 0.7 cfs

The total diversion-plus-bypass flow is about 5.3 cfs. The total rights on the creek are 9.48 cfs. Therefore, the total available flow = 5.3 / 9.48 = 56%.

**So, John is right, he is not stealing water!** He is taking 52% of his water right, when he could be taking 56% according to the “**sum of the boxes**” method. Not only that, but Amy could take more, the Samples should reduce their diversion, and the Minks’s could take a tad more. Well, that’s theoretical – Quint and Marcie Minks probably cannot seal up their dam completely, so there may be a little bit less flow actually available for diversion.