Soil Health: a Function of Time in Nature and Practice in Production Agriculture

Website Editor • July 5, 2017

If anyone has ever cleared off timber to open up new farm ground you can testify to the health of that soil and the impact it has on the early crops from that new farm. That’s a testimony to time and Mother Nature. Over time the balance and the state of the physical, chemical and biological property of the new soil came to be. Completely supportive, sustainable and self-perpetuating.   It isn’t until we take a step back a few years in passing that we realize that the heathy soil advantage is being impacted by our practice and cropping methods. Well I think we have all been in that scenario and have all had those same thoughts, wishing we could build that healthy soil again. In the length of my own career I have seen this revelation and more importantly I am seeing it swing back the other way and much of our work now is focused on rebuilding our soil health.  With so much talk out there about Soil Health it can begin to sound like a quick fix, just add a little of this and do a little of that and your all set. I wish it was that easy and the soils were that quick to respond! I don’t want to get into this too deeply, we’ll save that for another conversation, but I would like to touch upon a few basic thoughts on the subject. The truth is, Soil Health is as much about what you do as it is what you use! You see true Soil Health is a balance of soil properties. A healthy soil is one that has sufficiency and balance between the Physical,the Chemical and the Biological properties of the soil.  The Physical propertiesof the soil is about structure, the particle shape and size, the balance between sand, silt, clay and soil organic matter and the soil porosity. The Physical property is where the crop will find anchorage, the presence of oxygen, water, carbon and the storage of nutrient. Where symbiotic biology resides and where the fuel for growth is exchanged. Things that can decrease the physical soil attributes are poor aggregate balance where soils lack balance between the particle types and may possess too much sand, silt, clay or soil organic matter in proportion to the other components. They are soils that are too open or soils that lack porosity and can hold little water or oxygen due to overworked soil, soil worked too wet or due to flooding as many areas have experienced this growing season. There are practices that we can adopt that will support or improve the physical state of our soils and the first practice must be discipline! Resist the urge to make all of those historical tillage passes and stay off wetter soil until its ready. Consider Minimum or No-Tillage systems and strongly consider introducing cover crops into your practices. Cover crops can help us improve structure and build carbon back into the soil. Cover crops also penetrate soil layers and aggregates while supporting nutrient mineralization, repositioning and/or sequestration. Cover crops also provide a thriving environment for biology during the between season of agricultural crops. A healthy Physical soil structure will provide a place for the crop to grow, where roots can freely explore the spaces between soil aggregates and acquire the necessary components for growth. Chemical properties of the soil, in part, build off of the soil structure. The total exchange capacity of soil is impacted by the balance of soil colloids.  Sand, silt, clay and soil organic matter particles all have independently unique exchange capacities.   Nutrient balance and pH are key components to the Chemical property of soils. Soils without nutrient balance will not support effective nutrient exchange and will result in plant stress or nutrient deficiency.  An over present nutrient can act like an antagonist to other nutrients and impede nutrient uptake. A good example of this is too much calcium.  Too much calcium can and will complex with phosphorus forming calcium phosphate rendering both nutrients useless. It will also tend to push potassium off the soil colloid and if not taken up by the crop will expose the liberated potassium to precipitation through the soil profile, especially if it happens to be sandy in structure. Soil pH can influence this action dramatically! The pH of a soil can impact nutrient availability and overall soil health not only by promoting complexes but it will also have an impact on the solubility of many nutrients. A good example here would be iron! The plant uptake form of iron is a divalent form or a Fe2+ form. Iron residing in soils with a pH of 6 to 6.5 will support this Fe2+ form however if the pH is allowed to increase over 6.5 that Iron molecule’s state of oxidation will be altered and convert to a Fe3+ or even a Fe4+  form and the solubility of that iron molecule will decrease exponentially. At that point even if you can have an abundance of iron reported on a soil test you could still see iron deficiency in your crop. The natural tendency in soil chemistry is that a soil left alone to the devices of nature will over time find equilibrium. However a soil in crop rotation that is out of balance due to poor nutrient management, overproduction or the destruction of nutrient exchange capacity will tend to add stress on crops and impact overall crop production in that environment. The Chemical soil environment can also impact the Biological property of the soil! Soil Biology can reside in a wide range of soil environments, some forms of biology function better in a higher pH for example while others prefer a lower pH. Some perform better in soils with higher nutrient levels while others in lower levels. The scope and concentration of soil biology is a tender balance originating over many years and is very specific for that environment and indigenous plant community. In years past, our soils were more capable to recover from our cropping methods. We did less tillage in some respects, we added more organic matter back into the soil and in many cases fallowed and used more companion and cover crops. Our pesticide focus was different then and we used more mechanical means of weed control. More importantly we didn’t carry out as much and push our soils then as we do today. This realization has prompted many to seek methods of production today and choose products that support soil health. Even our industry as a whole finds value in this venture, so much, that great effort is being put into research, production and education towards the use of such products and methods. We’re having some impact with nutrient, traffic and tillage management and we’re now making headway with the introduction of biological inputs. We are harvesting more bushels per acre in some cases by recreating that healthy soil environment and managing the details, the small players in our production, the soil biology. NACHURS Rhyzo-Link is a product line focused on promoting soil and plant health. NACHURS Rhyzo-Link products are fortified with a cultured consortium of highly populated Rhizobacteria and are built with purpose, designed to restore and promote beneficial bacteria necessary for sustainable crop production. Not only is rhizobacteria needed in plants to support biological function, nutrient mineralization and assimilation but rhizobacteria have a role to play in soil balance and in soil health as well. Production practices and products to rebuild soil health may very well be the key to the future of sustainable Agriculture! You can find more information on our Rhyzo-Link products on our website at www.nachurs.com , from previous blogs or from any of our NACHURS representatives.

If anyone has ever cleared off timber to open up new farm ground you can testify to the health of that soil and the impact it has on the early crops from that new farm. That’s a testimony to time and Mother Nature. Over time the balance and the state of the physical, chemical and biological property of the new soil came to be. Completely supportive, sustainable and self-perpetuating.  

It isn’t until we take a step back a few years in passing that we realize that the heathy soil advantage is being impacted by our practice and cropping methods. Well I think we have all been in that scenario and have all had those same thoughts, wishing we could build that healthy soil again. In the length of my own career I have seen this revelation and more importantly I am seeing it swing back the other way and much of our work now is focused on rebuilding our soil health. 

With so much talk out there about Soil Health it can begin to sound like a quick fix, just add a little of this and do a little of that and your all set. I wish it was that easy and the soils were that quick to respond! I don’t want to get into this too deeply, we’ll save that for another conversation, but I would like to touch upon a few basic thoughts on the subject.

The truth is, Soil Health is as much about what you do as it is what you use! You see true Soil Health is a balance of soil properties. A healthy soil is one that has sufficiency and balance between the Physical ,the Chemical and the Biological properties of the soil.  

The Physical propertiesof the soil is about structure, the particle shape and size, the balance between sand, silt, clay and soil organic matter and the soil porosity. The Physical property is where the crop will find anchorage, the presence of oxygen, water, carbon and the storage of nutrient. Where symbiotic biology resides and where the fuel for growth is exchanged.

Things that can decrease the physical soil attributes are poor aggregate balance where soils lack balance between the particle types and may possess too much sand, silt, clay or soil organic matter in proportion to the other components. They are soils that are too open or soils that lack porosity and can hold little water or oxygen due to overworked soil, soil worked too wet or due to flooding as many areas have experienced this growing season.

There are practices that we can adopt that will support or improve the physical state of our soils and the first practice must be discipline! Resist the urge to make all of those historical tillage passes and stay off wetter soil until its ready. Consider Minimum or No-Tillage systems and strongly consider introducing cover crops into your practices.

Cover crops can help us improve structure and build carbon back into the soil. Cover crops also penetrate soil layers and aggregates while supporting nutrient mineralization, repositioning and/or sequestration. Cover crops also provide a thriving environment for biology during the between season of agricultural crops.

A healthy Physical soil structure will provide a place for the crop to grow, where roots can freely explore the spaces between soil aggregates and acquire the necessary components for growth.

Chemical properties of the soil, in part, build off of the soil structure. The total exchange capacity of soil is impacted by the balance of soil colloids.  Sand, silt, clay and soil organic matter particles all have independently unique exchange capacities.  

Nutrient balance and pH are key components to the Chemical property of soils. Soils without nutrient balance will not support effective nutrient exchange and will result in plant stress or nutrient deficiency.  An over present nutrient can act like an antagonist to other nutrients and impede nutrient uptake.

A good example of this is too much calcium.  Too much calcium can and will complex with phosphorus forming calcium phosphate rendering both nutrients useless. It will also tend to push potassium off the soil colloid and if not taken up by the crop will expose the liberated potassium to precipitation through the soil profile, especially if it happens to be sandy in structure.

Soil pH can influence this action dramatically! The pH of a soil can impact nutrient availability and overall soil health not only by promoting complexes but it will also have an impact on the solubility of many nutrients.

A good example here would be iron! The plant uptake form of iron is a divalent form or a Fe 2+ form. Iron residing in soils with a pH of 6 to 6.5 will support this Fe 2+ form however if the pH is allowed to increase over 6.5 that Iron molecule’s state of oxidation will be altered and convert to a Fe 3+ or even a Fe 4+   form and the solubility of that iron molecule will decrease exponentially. At that point even if you can have an abundance of iron reported on a soil test you could still see iron deficiency in your crop.

The natural tendency in soil chemistry is that a soil left alone to the devices of nature will over time find equilibrium. However a soil in crop rotation that is out of balance due to poor nutrient management, overproduction or the destruction of nutrient exchange capacity will tend to add stress on crops and impact overall crop production in that environment.

The Chemical soil environment can also impact the Biological property of the soil!

Soil Biology can reside in a wide range of soil environments, some forms of biology function better in a higher pH for example while others prefer a lower pH. Some perform better in soils with higher nutrient levels while others in lower levels. The scope and concentration of soil biology is a tender balance originating over many years and is very specific for that environment and indigenous plant community.

In years past, our soils were more capable to recover from our cropping methods. We did less tillage in some respects, we added more organic matter back into the soil and in many cases fallowed and used more companion and cover crops. Our pesticide focus was different then and we used more mechanical means of weed control. More importantly we didn’t carry out as much and push our soils then as we do today.

This realization has prompted many to seek methods of production today and choose products that support soil health. Even our industry as a whole finds value in this venture, so much, that great effort is being put into research, production and education towards the use of such products and methods.

We’re having some impact with nutrient, traffic and tillage management and we’re now making headway with the introduction of biological inputs. We are harvesting more bushels per acre in some cases by recreating that healthy soil environment and managing the details, the small players in our production, the soil biology.

NACHURS Rhyzo-Link is a product line focused on promoting soil and plant health. NACHURS Rhyzo-Link products are fortified with a cultured consortium of highly populated Rhizobacteria and are built with purpose, designed to restore and promote beneficial bacteria necessary for sustainable crop production.

Not only is rhizobacteria needed in plants to support biological function, nutrient mineralization and assimilation but rhizobacteria have a role to play in soil balance and in soil health as well. Production practices and products to rebuild soil health may very well be the key to the future of sustainable Agriculture!

NACHURS

By emily.bookless February 6, 2025
February 6, 2025 
September 18, 2024
The benefits of maximizing potassium efficiency
August 20, 2024
The benefits of Zinc on Winter Wheat
July 9, 2024
As I travel across Canada, it has been great to see moisture along much of my path. Greener pastures and ditches in Alberta, lush spring wheat, durum, and lentil crops in Saskatchewan, as well as many triticale, grass, and alfalfa fields, are being cut from British Columbia to Nova Scotia. I do not want to forget those potatoes spread across our country along with many specialty crops. As heat and moisture have brought germination, emergence, and vegetation growth, our crop nutrient management remains a key to success as we monitor the “Points of Influence.” Crop scouting, accompanied by tissue or sap samples, supports crop-based crop protection and foliar nutrient applications. As we have been programmed to concentrate on nitrogen, we are putting a lot of pressure on one nutrient to solve many deficiencies and concerns while ignoring the balance of fertility our crops may be looking for. In this blog post, I will not cover all the nutrient requirements but concentrate a little on magnesium, as I refer to what makes plants green. This spring, a significant amount of discussion surfaced around magnesium, and several growers requested magnesium for their cropping plans. Sometimes, what is new is old; looking back, magnesium has been a big part of many crop plans for decades. In sandy soils, specialty crops, and our high calcitic soils, we are looking to balance our oxygen and moisture space in soil levels. To better understand what we are looking at, I have included a list of what Mg is responsible for as well as soil activity stated: Magnesium Crops require magnesium to capture the sun's energy for growth and production through photosynthesis. Magnesium is an essential component of the chlorophyll molecule, with each molecule containing 6.7 percent magnesium. Magnesium also acts as a phosphorus carrier in plants. Necessary for cell division and protein formation. Phosphorus uptake could not occur without magnesium, and vice versa. Magnesium is essential for phosphate metabolism, plant respiration, and the activation of several enzyme systems.
June 11, 2024
Welcome to June 2024. As discussed in our March article, weather is what we receive from above, and we do not make the arrangements. Again, what is in our control is taking our past lessons and applying our experiences to the 2024 crop. As we continue to “learn, unlearn, and re-learn,” we can better understand the points of influence that we can utilize to react to our crop's needs. With most of the germination and emergence behind us, we are looking to drive vegetation by developing the best foliage we can, capturing maximum sunlight, and amplifying plant energy. This energy will be the key to supporting reproduction and then crop fill throughout the season. This is where tissue and sap sampling must be utilized to build a balanced foliar program. Once we understand a crop's requirement, we can look at a demand curve and design a program to enhance plant health. Foliar applications are often a rescue, and not in the plan, as a tool, but are very valuable in utilizing soil-applied fertility through root activation. To better understand foliar applications, we must understand what we want to achieve. First, we need to have nutrients that can be taken up by the plants. Second, we need to understand how we will feed the plant, and thirdly, we need to apply fertility with a purpose. When applying foliar products, the rates will seem inadequate for the deficiency, but what is the overarching goal? “One of the touted benefits of foliar fertilization is the increased uptake of nutrients from the soil” (George Kuepper, NCAT Agriculture Specialist, Foliar Fertilizer 2003). As we continue to learn more about root-to-soil interaction, the measurement of root tips leads to a better understanding of how each tip, expressed through foliar applications, amplifies nutrient uptake. Regarding plant fertility, our ALPINE foliar products contain orthophosphate, which plants can readily absorb through vegetation. The potassium source, ALPINE Bio-K, has the benefit of smaller molecular size and a low deliquescence point, extending available uptake time. The ALPINE Micronutrients are also chelated, allowing them to be available for uptake by the plant. As for foliar feeding your crop, we want to apply products when the plant is best available to receive them. In the mornings, when the stomata are open, stay away from the day's heat stress. If a foliar dries on a leaf, it must re-wet to become available again. It is also advantageous to feed a healthy crop and fend off stress instead of waiting to see the stress and deficiencies prior to a reactive application. It is also essential to understand how nutrients move via diffusion. So, when we can keep our foliar fertilizer in solution for a more extended period, the concentration increases during water evaporation, allowing the fertilizer to be taken into your crops. Applying with a purpose is what I continue to strive to learn, causing me to read, experiment, and incorporate new ideas along the way. Take our ALPINE K20-S, for example, a 3-0-20-8S-0.2B-0.1Mn-0.002Mo blended foliar. Nitrogen works as an adjuvant to enhance nutrient uptake and increases the formation of amino acids required to develop protein along with sulfur and molybdenum. The ALPINE Bio-K, a potassium acetate source, increases plant metabolism, nutrient uptake, and feeding microbiology. As a result, the package, which also includes boron, is designed to improve uptake and assimilation to better equip your crop for success. When combining ALPINE K20-S with ALPINE CRN-B later in the vegetation season, we can stimulate crops to greater success. If the rain continues, this combination has proven to strengthen crops struggling with root rot and K & B deficiencies. I would also like you to consider working with your nitrogen applications, knowing that straight N is not always your plant's best friend. As we continue to look at humic and fulvic acids, along with Boron, Magnesium, and Calcium, in blended situations, there will be much more to write about in the near future. If you have further questions, don't hesitate to contact your ALPINE DSMs and Dealers. I wish everyone a safe and prosperous Summer ahead. Steve McQueen, Agronomy Manager
May 23, 2024
The Amplification of ALPINE F18 Max
ALPINE Liquid Fertilizer Blog
March 21, 2024
The movement to ALPINE’s newer in-furrow starter, ALPINE G241-S continues to happen across Eastern Canada...
March 6, 2024
ALPINE Bio-K Enhanced Feed Quality
More Posts
Share by: