Over the past year I have been researching methods of improving my garden soil. Living on a Glacial moraine my property soil texture is made up normally of about 30%rock and boulders, 60% sand and about 5% silt with no measurable amount of clay. Even though we have added considerable organic via composting over 20 years, the majority of our soil does not readily absorb or retain moisture. After a 1” rain during summer I can find powder dry soil at 1/4” deep! So needless to say plants that are not very well mulched do not grow well. Adding commercial fertilizers does very little since plant roots also need a soil structure that breathes well and allows moisture retention that support cation exchange to fully metabolize soil nutrients. My soil generally fails that test! Hence my efforts to improve it!
The below article by Purdue.edu describes the benefits of improving the CEC of soil and explains why “clay” the missing constituent in my soil plays a key role in the CEC of any soil.
https://www.extension.purdue.edu/extmedia/ay/ay-238.html
So I set out this week to determine where in Washington state one can obtain quantities of clay. After reading the below article published by department of natural resources, I set out to find a local source.
Pg 144 of the publication describes Hammer Bluff: is in the NE1/4 sec. 28, (21-6E) as a 38 foot face formed by the Green River impinging against a short spur that projects from The Valley side. The layer of clayey sand at Hammer Bluff measured 12’ deep when the geologist visited this site.
Since this location is within 30 minute drive I went to determine if this source is available now to the public. After locating the site on a roadmap I determined to visit Flaming Gyser State park that borders the Green River. At the headquarters I met a park ranger who was familiar with the site and gave me precise directions to find Hammer Bluff. As I followed his direction walking downstream just outside the Park boundary, I came to a spot where looking up from the valley floor at about 1/4 mile away and about 600-700’ above the valley floor stood the sheer vertical outcropping of Hammer Bluff. The face of the bluff shone all the colors of the rainbow. As I observed this spectacle it occurred to me that once upon a time in our geologic past, the flows coming down the Green River gorge has dislodged the materials causing a huge landslide that must have filled the entire valley floor with huge volumes of rock, sand and clay.
As I reflected on how many years the Green River has been transporting these sediments to valleys below, it became clear to me why the alluvial soils in the valley that spans some 60 miles from Auburn to the mouth of Green River where it’s spills into Puget Sound are so abundantly fertile.
So I went about collecting samples of the local clay materials along the bank of Green River near Hammer Bluff.
The results of two samples I collected were as follows when I ran a simple fruit jar shake test.
After 24 hours the below pic shows how the constituents (sand, silt, and clay) measured in their respective proportions. Left to right: sample on the bank at about 10’ above water surface of the river, sample of the topsoil about 50 meters away from the river, 50/50 sample of the river bank clay mixed with my native property soil) :
Below is a picture of the third sample on the right above before I added water: 50 % of my property soil on the bottom and 50% of the riverbank clay on top:
The proportions of each soil constituent of all the samples were measured as:
My native soil:
Sand = 2 and 1/8 = 18 eights= 90%
Silt and clay 1/4” = 2 eights = 10%
Left sample Riverbank clay:
Sand = 1&3/4” = 14 eights= 53.8%
Silt = 3/8” = 3 eights = 11.5%
Clay= 1&1/8” = 9 eights = 46.1%
Middle sample away from riverbank clay:
Sand = 2” = 16 eights= 53.3%
Silt = 1/4” = 2 eights = 6.7%
Clay=. 1& 1/2” = 12 eights = 46.6%
50/50 sample of Riverbank and my property:
Sand = 2” = 16 eights= 66.7%
Silt = 1/8 = 1 eight = 4%
Clay 3/4” = 6 eights = 25%
Organics= 1/8” = 1 eight= 4%
By merely mixing 50/50 my property’s native soil with an equal volume of riverbank clay the classification goes from sandy soil to sandy loam on the Soil Texture classification triangle! As I took those measurements today I was elated to see that I now have a way of achieving a very high quality soil amendment by simply importing more valley clay. The way forward is now very promising, by adding valley clay and tossing in about 5% compost or other organics I can create a very fertile topsoil mulch for those places where I want to improve fertility and soil moisture naturally.
Dennis
Kent, wa