Sabot L'ours (sabotlours) wrote,
Sabot L'ours
sabotlours

Data

It seems that it was just a few days ago that I posted about starting a study on how the housing developments on the mesa would affect the drainage system up there. On Wednesday night I was able to get my first data point! We had a nice typical monsoon storm roll in about dinnertime. Up until now the rains have come in from the north and at a later time. I always remembered the storms rolling in just as I left work, not just before bed. So I was able to enjoy the wrath of the storm as it dumped sheets of rain in a relatively short time. As soon as it slowed to a drizzle, I headed up the mesa to check on my drainage ditch. It performed perfectly! It deepened in many places and became a little more well established. I'm still dealing the with slope issue since as soon as the flow slows down, it deposits sediment. Oh well. I can help things out by removing a few shovelfuls of sand to keep the slope adequate. I then decided to hike up on the mesa to check out the arroyos I am wanting to study. As I hiked over to the main channel, my heart skipped a beat. Was that running water that I was hearing?!? I made a beeline for the "waterfall" I had mentioned in the previous post where it looked like water spilled over the mesa and down a heap of rubble. It was flowing! I don't know how many people have ever witnessed the sight, but not only did I see it, I captured it on video!



I was a bit surprised to see that there wasn't any water in the arroyo. What was going on?!? I then realized that the flow had only started about a minute before, and soon a lobe of water began flowing downstream. I captured that on video as well.



I then followed the flow upstream to see what was happening. There was good flow coming from the detention basin to the west. That was meeting up with flow coming from the detention basin to the north. In some places there was a well-established channel. In some places there was insufficient gradient, so the flow spread out in sheet flow. I made my way up to the concrete channel that leads from the north detention basin. It was flowing pretty good. There was definitely some erosion going on. I then got something of a shock when I realized that the new development to the north would also be draining into the detention basin. That will be adding a significant volume of water to the mix! But then again, the outflows are pretty much restricted, so the flow rate might not be significantly higher, but the flow duration might be. The other modification to my hypothesis is that there may not be significant erosion in the future due to control points. There probably will be channel establishment just below the detention basins, but due to grade controls, it shouldn't be extreme. The waterfall will act as a control point since it will take a lot to erode bedrock. Just below the waterfall there is a narrow bedrock canyon which will also act as a control point. Finally there is a stretch of arroyo that is fairly flat just below the canyon. Velocities should be low since it appears so flat. The channel then goes under a road bridge which I noticed has a concrete lip underneath it. That will also act as a grade control to prevent significant erosion. So basically my study will focus on the development of channels over time as they react to greater volumes. There should be a geomorphic response since you're now putting flow down a channel perhaps 5 times a year when in the past there might have only been flow down the channel once every 5 years.
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