Erosion is the natural state of New Mexico’s watersheds. Although this may be said of any watershed in the world, it is particularly appropriate on a relevant time-scale in the desert. Erosion in some areas of the world may take generations to be noticeable. Here, the conditions are such that rapid erosion is the natural and normal state of things. In Craig Childs’ book The Secret Knowledge of Water, he experiences incredible changes in topography over a period of hours or even minutes in the southwest. The dry barren landscape can be exposed to a sudden deluge of rain, and the resulting flash flood can carve the landscape quickly.
Precipitation is so infrequent that many watersheds do not have constant moisture, and moisture levels are not adequate to support dense plant cover that would hold back soil. There are riparian areas with dense plant cover, but these areas areas are usually relatively small areas, that are surrounded by low density vegetation. When water flows, it flows in a devastating torrent.
The substrate in this part of the world can hardly be called soil; a more accurate description would be sand, or gravel. The larger sizes don’t have enough surface area for water to adhere them together, even if there was water. The finer sands don’t have moisture or organic matter to bind them, and the winds easily blow them around.
This is what is considered "soil" here:
My daily walks frequently take me past areas where designed drainage systems are not functioning well. This landscape was installed just a few years ago. See what it looks like today. Keep in mind that all of these photos (except for the few noted below) are on the same short stretch of road in my neighborhood.
This has cut down more than a foot.
Can you find the drainage grate? It's under there.
I bet they thought that if they buried the PVC pipe 15 inches down, that it would be plenty.
Roadsides are particularly vulnerable, especially on a slope. There is all the run-off from the impermeable and large surface area of the road, and the slope increases the rate of flow.
Here's another drainage grate. See how the water flow from the road is cutting under the concrete?
This is the roadside off a dirt road getting to a hiking trail. Runoff does things, doesn't it?
Another view of the same cut:
In this area, they've tried to stabilize the roadside with cinder block. See how well it works. Isn't it beautiful?
Volcanic rock:
Graded river rock:
Naturally planted swale (i.e. "weeds"):
Half-buried stone on half the swale:
Chain link fencing:
Stone lined swale (installed last year):
Double asphalt (installed last year):
Riprap swale (installed about 4 months ago). You can see what happens to this type of swale when it rains - the water moves faster at the edges than over the rocks, cutting down the soil. The water-borne sand falls out of the slower moving water over the rocks. In another few months, this will be an elevated rockway, and during rains, the water will be flowing only on the cutdown sides. You see this all over Albuquerque.
Another view of the ineffective riprap swale, with downcutting on edges, and filling with sand. Keep in mind, that this is only 4 months later.
The riprap drains into this loveliness:
Which drains here. Note how well the edges are holding up (again, 4 months later), around the concrete.
So how to design better drainage systems?
If we remember how natural water drainage systems work, we remember that it is a constant state of erosion. Through these systems, rock, in the form of sand and gravel, is constantly flowing down off our young steep mountains. To stop that is impossible.
There are a few techniques that are now used, as you see above:
1. Facilitate flow. This is done by creating drainage lined with concrete or asphalt, to sluice away any water/gravel. Problems: no ground water infiltration, systems fail, usually at one end or another, but also along the route. Environmentally/ecologically it is a mess.
2. Allow flow with ground infiltration by creating a static channel. This is often done by bank stabilization using rock or concrete block. Problems: you see what happens in the photos above. Not pretty, and frequently not effective.
3. Allow flow using creating a more dynamic system to stabilize the channel: done using plantings. Problems: still allows some downcutting, and the channel is not predictable in a tight area. Can plantings be established in time for effectiveness? What plants are best suited? If the natural landscape does not support dense enough plants, will a roadside swale support dense enough plantings?
The first method is clearly the worst. The second method doesn’t work well at all. The third method is questionable as well.
Can we propose a new method? Whatever the method, it needs to be dynamic enough to allow natural processes to occur, and static enough to allow for road construction...or, do we have to have roads? It would be cost prohibitive to built raised roadways that allow natural erosion beneath. Maybe we need non-polluting hovercraft. I've seen new drainage designs mimicking natural flows in my classes. It's the latest thought on roadside drainage.I wonder how they would work here? It's too late to implement those in this neighborhood though.

