White Paper: High Resolution 3D Mapping of Aquatic Habitat at the River Corridor Scale .

Click on the link below to open a .PDF of the white paper presented at Hydrovision 2018.

Martoz and Lorang 2018 HydroVision

Sacramento/San Joaquin Delta 3D Mapping Project

In October of 2017, the Freshwater Map team traveled to Sacramento, California to take detailed measurements of the Sacramento River from Clarksburg to Isleton, about 21 river miles.  We measured the bathymetry, 3D flow, temperature and hundreds of other parameters over the same reach on three consecutive days to determine how the river changed over the tide cycle.  On the fourth day the team measured up and down 10 miles of Elk Slough, which showed some very interesting ground-water/surface water characteristics due, we suspect, to levee permeability.

Over the four days of data collection each of our eight river technician’s systems pinged twice each second.  The total dataset quite large (over 1.8 million records).  A link to a .pdf of the full report is below.

Please contact us with any questions.

dane@freshwatermap

Technical Report – Sacramento River Delta 3D mapping project

Scientific Article – Journal of Applied Ichthyology

Click on the link below to read the summary and access The Journal Of Applied Ichthyology research paper.

http://onlinelibrary.wiley.com/doi/10.1111/jai.13569/full

Flathead Lake Habitat Enhancement

North shore Flathead Lake at mouth of Flathead river

 

Freshwater map has been working on Flathead Lake for many years.  Our latest project focused on erosion control at the north end.  High water levels during winter storms had been causing erosion on the north shore as southern wind-driven waves hit the gravel shoreline.  Freshwater Map designed and managed the installation of dynamic revetments on the shoreline that reversed the erosion caused by the wind-wave action.  After installation, woody debris and other organic flotsam has deposited on the shoreline, which, through continued wave action, has broken down into permeable peat.   The permeable gravel and peat has accreted the shoreline while still providing sufficient seepage and over-topping to fill a shallow-water rearing habitat and wetland behind the shoreline.

Arial photos with the 2005 and 2016 waterlines shown. The large (5.46 acres, also shown as orange areas in figure 5) creation of new wetland habitat on the west side of the river is due to the small gravel spit constructed near blue arrow. Similar new habitat has been created (5.16 acres also shown as orange areas in figure 5) behind the offshore structures and along the shores further to the east.

Design options considered by the landowner included shoreline hardening at a much higher cost that was much more difficult to install and would have resulted in many unintended consequences due to wave reflection off the hardened shoreline and no wetland habitat improvements.

This is a single example of Freshwater Maps work on Flathead Lake in Montana.  Over the years, we have designed and built over 2 miles of protective shoreline, all of which utilize dynamic structures made of natural materials.  Our designs enable the wind and wave action to do the work of building effective protection of property while enhancing habitat.

Contact us to discuss removal of shoreline hardening to enhance habitat and shoreline protection.  (406) 420-2295

Dry Creek, Sonoma County, CA

 

Dry Creek is a tributary to the Russian River in Sonoma County in Northern California’s wine country.  The relatively short (12 miles) trib runs from Warm Springs Dam to the Russian just west of downtown Healdsburg.  The deeply incised channel runs through spectacular vineyards and, in the past, has been the site of gravel mining and other habitat challenges.

The Sonoma County Water Agency, working with the Army Corps of Engineers, is working to augment habitat on the reach to provide flow refugia for steelhead trout and coho salmon.   The stream is a challenging one due to flood control issues and large variances in the annual hydrograph.  Summer flows are in the 100 cubic foot-second range (CFS) while winter storm flows have been measured above 5,000 CFS.  The creek bed is made up of gravel, mud and occasional cobble which makes for a very dynamic channel that can change dramatically in a single season.

Last season’s heavy rains caused a much woody debris to fall into and across the river…but our team prevailed!

Dry Creek Obstacles

Freshwater Map provided over 60,000 data points within a 1.2 mile reach of this stream.  These data include depth, flow velocity and 3D vectors to help our client design flow refugia and channel complexity that works with the natural forces in the channel.  It’s an example of our strong belief that when we understand the river’s natural forces, we can better design augmentations that optimize the work the river is already doing.