Friday, December 24, 2021

GROUND TEMPERATURE --Cultivated vs Uncultivated ground

 I'm redoing a study I did back in 2015-2016 on temperature differences in different ground conditions.  Those earlier findings can be seen by clicking on "tests" in the labels section and scrolling to the bottom to "HOBO Temperature Sensors" posting.

This current study is starting on 12/24/21 in near freezing, snowing conditions. Temperature readings will be taken every 2hrs until we start seeding the spring crop in spring of 2022, around April.  There will be an update to this posting after seeding.  I started this study by spading and working up two areas to replicate a cultivated field with little surface residue.  I'm comparing this with field conditions where there is surface residue left undisturbed.  All the sites are within throwing distances of one another, one in long term CRP ground and the other in ultra low disturbed no-till crop ground.  We have had some variable weather ranging from freezing to thawing, and mixtures of rain and snow for the past week.  The field aspects are similar from one site to the other.  One difference showed immediately.  The worked CRP field had no sign of frost(pic upper left showing a lot of living roots), where the cropped field showed frozen soil about an inch deep (pic lower left showing some non-living roots).
These observed conditions support the idea that there is more biological activity in the CRP field where the grass roots are living, hence a warmer microclimate in the root zone, compared the the cropped field where there has not been living roots to stimulate biological activity for five months.  Biological activity creates heat.
    HOBO temperature/light sensors (model UA-002-08) will be placed on the surface and at the 2" depth in the cropland sites.  This is my primary interest, to see if there is a temperature difference between cultivated and uncultivated ground, both surface and subsurface locations.  The inclusion of CRP ground is to see how ground temperatures differ between cropped ground with it's limited time supporting living roots, and ground that continuously supports living roots. 
     Once put in place, these sensors will stay until recovery in early spring.  They don't support remote monitoring or downloading. 

The pic to the left shows a typical plot from the data collected with the HOBO (UA-002-08) sensor for temperature and light. A (HOBO) sensor and the "reader" is shown above the wireless keyboard and trackpad.

Tuesday, June 22, 2021

Tillage to Reduce Herbicide Resistance

 A recent posting in "Weeders of the West" a WSU blog [https://smallgrains.wsu.edu/weeders-of-the-west/2021/06/21/occasional-tillage-and-herbicide-resistance/ ] stirred me to make this posting.  The link above will take you to their posting that I am referencing.  For about 5 years I have been hearing WSU weed scientists introduce "occasional tillage" back as a practice to reduce herbicide resistance.  For those of us that are die-hard no-tillers, that's like throwing gasoline on a fire, --it makes no sense what-so-ever.

      I could rant on this all day, but I will try and limit my comments to a few references in the posting.  I’ll start with a statement of my position.  I’m not quite as old as dirt but I was around before there were synthetic chemistry or fertilizers for our crops.  I have spent most of my life stirring dirt, destroying my little portion of the Palouse ecosystem.  For the last 30 years I have been trying to figure out how to repair that damage.  Since the year 2000, research on soil health has grown astronomically.   It's to the point where I discount (not reject) research findings that are more than 5 years old.

--What is soil health?  I find that it has many different parameters depending on who is speaking on the subject.  I can accept Huberto Blanco-Canqui’s findings for the high quality, deep soils that probably make up their research sites.  If the soil is deep, with high OM, and a near neutral pH, then, an occasional stirring probably is a minor setback to the ecosystem.  Soils with a high level of biological life have the capacity to rapidly rebuild after a destructive event.  Soils with low levels of biological life do not have that capacity, so rebuilding is slow.  The post mentions tillage to break up compaction and reduce stratification of soils.  Back in the 70's, WSU was researching ways to mitigate tillage compaction. Compaction was recognized as a problem through the use of moldboard plows, disc harrows, and rod weeders.  I had fields where four tillage pans could be identified.  Chisle plows and heavy cultivators were proposed solutions.  Compaction layers were found to be moving lower in the soil profile because chisels and cultivators broke soil aggregates into finer particles that moved deeper into the profile.  Deep chiseling and subsoiling was considered, but rejected because it was feared that compaction layers would move lower than implements could reach.  We are still dealing with compaction layers in our soils.  It has been demonstrated that we can influence compaction and stratification of our soils with plants and biology.  We need to figure out how to incorporate them as part of our cropping practice.  There are plants and macro fauna that are very good at these tasks and leave a better long term effect.  Except for small acreages, soils in the Palouse, in general, are badly degraded from erosion from years of cultivation (erosion from cultivation, water, and wind), and from being mostly a monoculture cropping system.   Any cultivation is a major setback to our ecosystem.  I compare "occasional tillage" to burning your house down every few years.  Many of the soil biological structures don’t rebuild very quickly in our climate and cultural environment.  Tillage and fallow is a real downer for soil microbe communities.  Biological networks are sliced, diced, burned, starved, --and are slow to recover from a major disruption.  

--What is “occasional cultivation”?  I have never heard a followup explanation as to what this term meant, or how it would extend a herbicides useful life.  Retracing my memory of tillage I don't think there is such a term as "occasional cultivation.  Nearly every year I see a farmer do reduced tillage, and weed escapement is always a problem, which results in more tillage, or chemistry applied with less than desirable results.  My experience is that tillage bury’s seed, of which some emerge and the remainder stay in the soil bank, safe, for later emergence.  Tillage destroys OM and emits CO2 and H2O into the atmosphere. Tillage degrades the soil through erosion, compounding our problems.  I find that, the less the disturbance, the fewer the weeds that compete with the crop.  I regularly see this in my fields.  A mat of surface residue along with no disturbance is preferable.  I often wish my equipment could levitate over the fields leaving no track.  Wheel tracks are where the weeds are.   An expanded crop rotation, and rotating appropriate chemistry will be more effective than tillage in reducing herbicide resistance in weed populations.


        --The ultimate goal will be removing synthetics from crop production.  As time passes this will happen because of weed resistance, environmental regulation, or cost.  These pressures will force us to learn to incorporate cover crops, do inter-seeding, and use companion crops in our production of cash crops.


        --Disciplines within soil & crop sciences need a closer relationship.  Weed scientists need to look for solutions through microbiologists, crop specialists, and other related disciplines.  Books like “When Weeds Talk” by Jay L. McCaman have a lot of potential for weed management, by manipulating soil chemistry and biology through plant cultivars.  Research by crop specialists working with cover crop cultivars, intercropping, and companion cropping are showing some real promise in increasing yields and reducing weed competition and diseases in cash crops.  Cropping problems need to be approached through coordinated discussion and research by cooperating disciplines instead of individual disciplines reverting back to old failed practices. 

Tuesday, May 11, 2021

Soil Field Condition vs Lab Tests


These pics are examples of WW crops from two different tillage systems.  Both of these crops look pretty good as of April 13th, 2021.


<-----  Pic on the left is an example of 2021 WW on long term conventional ground.  This  crop was seeded on chemical fallow grnd.



<---- Pic on the left is an example of 2021 WW on ULD grnd.  This area was seeded too shallow and got a late start.




        This winter/spring I had a unique opportunity to run a lab test on two soils that have very different history.  One soil has ~30 years of no-till, with the last eight years being ultra-low disturbance no-till.  The other field, a couple hundreds yards away has a history of one hundred plus years of conventional tillage/cropping, with no no-till history.  Both locations were fairly level with low erosion from weather, although a difference in tillage erosion would be apparent.  The no-till field has a large amount (mat) of residue, and the tilled field has a small amount (a lot of open ground) of residue.   I had high expectations of seeing a dramatic difference in OM, EC, BD, Respiration, and some differences of several macro and micro nutrients.  WHAT A DISAPPOINTMENT!!  Some numbers were the same, and some showed slight differences, but all in all, no revelations.  This lab is not the general run of the mill type that we are all accustomed to.  I have used this lab for a couple of years for different projects. 

    Physically there is a world of difference between these two fields.  April 13th with no measurable rain since March 23rd the ULD grnd was soft to walk across, where the tilled field was hard under foot.  Sinking a 1"diameter soil probe into the ULD field was easy, down the full 4 ft length of the probe, where the conventionally tilled field was very difficult down to ~18", where resistance eased up (maybe even softer than the ULD field in the lower 2'.

        Why didn't the lab show differences as expected?    Two things come to mind.  1)- In my mind this was such a no brainer that I was careless taking the samples.  My process of taking an undefined slice of soil using a narrow trenching shovel was bad technique.  A lot of possible error could result.   2)- This supports my comments on earlier posts about lab testing, and difficulty in trying to show value of no-tilling through our long recognized lab protocols. 

     I'm convinced that no-till deals primarily with the physical component of soil health, but secondary to other processes like biological diversity and nutrient recycling.  Biological activity has to be helped with cover crops and possibly reintroducing microbiological species through well prepared compost and compost teas.   No-till is significant in improving soil drainage, and it reduces destruction of soil organisms community life.    No-till is the first step required for us (in the Palouse) in developing a healthy soil.  With few exceptions, our environment will not support tillage and develop a healthy soil.   Comparing infiltration rate, wet aggregate stability (SLAKE test), visual soil structure, and earthworm count is easy to do and shows dramatically what no-till brings to the table relating to soil health.  Bulk density should be an easy comparison, but the penetrometer is effected by moisture content, soil type and other factors that vary from point to point.   So, what do I conclude?  As many of my earlier posts mention, a no-tillage farming system, is very effective in building soil structure over time.  A no-tillage farming system, when coupled with high surface residue (soil armor) is very effective in controlling erosion from tillage, water, and wind.  A no-tillage farming system is helpful in slowing evaporation when coupled with a protective mat (soil armor) on the ground, and even more effective if also coupled with standing stubble.  Moisture is lost principally through evaporation, not crop production.  Keeping soil surface temperature down, and a low wind velocity along the soil surface, saves moisture that can be used by the crop.  Another benefit to a no-tillage system and heavy mat of residue is reduced competition from weed species, either broadleaf or grasses.  We see it consistently year after year when comparing our neighboring fields with either conventional tillage or high disturbance no-till.  Unfortunately, we still have to apply herbicides like everyone else.

Value of low disturbance Direct Seeding

I had the opportunity to compare a field with long term low disturbance direct seeding history with a bordering field having a 100+ year history using a conventional tillage system. 
The pic on the left represents the field with the 100+ history of tillage.  The pic below (middle) represents the field with a long history of low disturbance direct-seeding.  In 2020 both fields were in chemical fallow.  The field in the top pic was chem fallow on spring wheat stubble. and seeded with a high disturbance drill.  The field in the middle pic was chem fallow on spring canola stubble.  It was seeded with a low disturbance drill.

  Observation:  Both fields were thawed.   This condition followed 10 days of hard freeze that provided ice sufficient to skate on our pond.  A quick thaw followed.  The field (top pic) was squishy, wet underfoot.  The near-surface was well above field capacity for moisture.  My loafers were mucked some when walking over the field.   The field (middle pic) was firm, indicating water moved down into the profile leaving the near-surface soil near field capacity for moisture.  Along with the surface armor, there was no danger of mucking up my loafers anywhere in the field.  I could have driven my F150 over this field.    

     The pic to the left (bottom) shows a part of the same fied that has a long history of conventional tillage.  Shown is winter wheat stubble that is cut very short.  This field is likely to be chem fallowed in 2021 and seeded to winter wheat in the fall of 2021.  This stubble area is soft and mucky on the top 2" and frozen below 2", making it difficult to walk.  The recent 0.29" of moisture (snow/rain) that helped thaw the surface is held in that top 2".  I was able to compare this condition with a field on it's border with tall standing stubble that has a long history of low disturbance direct-seeding.  That field was thawed and firm underfoot indicating that the 0.29" of moisture (snow/rain) had moved deep into the soil profile leaving the surface firm and near field capacity for moisture.
     These field areas are close together and likely received the same weather, so what is making the difference in field conditions?   Two possibilities come to mind.
    1) there is no question that the soil structure is improved providing more porosity (lower bulk density) in the long term direct-seeded field compared to the long term conventionally tilled field.  The slake test would easily prove that; however, in winter, with freezing or frozen conditions, soil structure with more porosity isn't the full answer.  
    2) There has to be a temperature factor involved.  How does this factor in?  Well, --there is 34 years where our direct-seeded fields have reduced or eliminated erosion compared to conventionally tilled fields.   That's nearly a 1/3 of the time since native grass was removed from the landscape.  That time has to have an impact on soil organic matter loss (SOM).  Add to that, the time that SOM may have been building since 2010 with the introduction of our ultra-low disturbance no-till system, which includes the stripper-header, expanding our rotation to add more crop diversity, and beginning the introduction of cover crops.   My bet is that we have been able to improve our "soils health" to the point that we are getting more biological activity.  More biological activity results in more heat which in turn warms the ground resulting in faster frost melt, and along with increased porosity, allows moisture to enter deep into the soil profile drying down the surface soil to field capacity.

    I have yet to followup by doing some simple tests, and I have missed the timing for the temperature component of my theory.  My HOBO's should have been in the ground last fall and left until now.  There are several simple physical in-field tests that can be done now that indicates a comparison of bulk density and soil porosity.  I hope to get them done this spring/summer.

    

    
   

Wednesday, January 20, 2021

FARMING NATURES WAY

USDA is a great resource to start the process of improving soil health on the land we steward.