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10/29/2024 - 22 min read

Soil Biology Testing Essentials

Featuring sampling guidelines, resources for interpreting the Soil Biology Report, and insights from the field

The Soil Biology Report

Understanding the microbes living in your soil is crucial to developing a holistic nutritional solution for your field. Soil microbes act as the engine for soil health by cycling nutrients, shaping soil structure, and promoting crop resilience by producing plant hormones. In this way, soil microbes help crops grow and protect them from stresses like drought.

Microbes both store nutrients in their biomass and help to convert decaying residues into nutrients that crop roots can use in a process called mineralization. However, while some soil microbes help crops, other microbes reduce nutrient availability through processes like denitrification, which causes nitrogen loss to the atmosphere. Soils that are more balanced between microbes that cause nutrient loss and conservation can provide greater nutrition to crop plants.

Understanding how well a field’s soil microbes can cycle nutrients and how they are balanced between nutrient loss and conservation can help us use fertilizers more efficiently. With enough knowledge, we can promote favorable microbes and mitigate the effects of unfavorable microbes to optimize crop nutrition.

The Soil Biology Report provides the tools needed to identify underlying causes of field variability, validate how products work in a field, and make decisions to maximize soil health. Our approach uniquely focuses on measuring the functional genes microbes use to cycle nitrogen, phosphorus, and potassium to show what microbes are doing in your soil. This approach is more precise, comes at a lower cost, and is designed to fit into your normal soil sampling process.

Soil Health Venn Diagram

As of Spring 2024, the Soil Biology Report also includes tests for sulfur-cycling microbial genes and reflects how you prefer available P to be reported (Olsen/Bray/Mehlich). In the coming years, the Soil Biology Report will continue expanding, with plans for new markers in 2025.

This article shares insights from the 2023 field season, explains the “why” behind sampling for soil biology, and shares resources around how to sample for soil biology, incorporate soil biology testing into trials, and interpret the Soil Biology Report.

Diverse soil biology leads to many benefits

Testimonials

Reese Martin, Loveland Products

“The way I see soil health… it’s a large factor in our agricultural production. I think it’s an area that we overlook.”

“We have an opportunity now with Waypoint not only for our tissue, our leaf, our soil sampling, now we can actually look and see and quantify what impact we’re having on our microbial community.”

“We have to protect the soil, the soil health, in order to continue to produce in agriculture, whether it’s a tree crop, a row crop, or a specialty crop.”

David Doonan, Nutrien AG Solutions

“It started with a goal to create a best-in-class customer experience, with an effort to help our growers reach their operational goals [and] to grow our LPI business by providing sound agronomic recommendations that are data driven and backed by science.”

Rodney Ratzlaff, Loveland Products

“We know we have a basic soil report, but that only gives us so much information. Soil biome takes that soil report to the next level with being able to understand specific microbiology that’s lending a hand toward NPK and even micronutrient use efficiency.”

“What excites me about this is that we’re dialing in specific recommendations per field and being able to give a lot more accurate recommendations from crop nutrition and building a more holistic crop nutrition program.”

Shane Van Fleet, Nutrien AG Solutions

“It has really shown me that we have the technology available to get the max efficacy out of products, and refine product application while improving soil health... We now have the ability to place the right products on the right farms.”

How Does Soil Biology Testing Work?

The order of operations for biology testing

How to Sample For Soil Biology

Waypoint’s soil biology test is designed to fit into your normal soil sampling process and requires no special equipment.

Two common reasons to test soil biology are (1) to diagnose potential issues in a field and (2) to evaluate how a product or program changes a field’s soil biology. Consider the following if you are interested in using soil biology testing for either reason.

How Many Samples Should I Take?

If you want to use soil biology testing to better understand and address issues in your field, we recommend taking 2–3 samples from areas that represent, for example, low-, average-, and high-productivity parts of a field.

If you are testing soil biology to trial products or practices, we recommend deciding between either (1) a simpler demo approach or (2) a more intensive trial setup.

For a demo approach, we recommend sampling both the grower standard and each treatment over at least two timepoints: before and after product application (i.e., 4 samples minimum). We have generally seen the clearest difference between treated and untreated samples at 2–6 weeks after product application. There could be reason to sample outside of that time window, so feel free to contact Waypoint with questions about sampling.

If you are interested in conducting a more intensive trial, we still recommend sampling over at least one pre-treatment and one post-treatment timepoint, but you may also consider sampling at additional post-treatment timepoints (e.g., at 0, 3, and 6 weeks after application) to better understand when products yield the strongest effects on soil biology.

A more intensive trialing approach will most importantly involve replication. To create a randomized complete block design, we recommend first dividing your field into as many “blocks” of equal size as there are replicates. Three replicates is generally considered a minimum.

Divided field into equal blocks

Next, divide each block by the number of treatments and randomly assign treatments to plots within the block. In the example below, the blocks have been split in half for the two treatments. Assigning treatments randomly rather than placing them on, say, the north and south sides of a field, will help minimize the chances that field variability (like a more acidic south half of the field) affects your results.

Blocks with random treatments

In the figure above, one composite sample (i.e., one bag with 8–10 cores), would be taken from each of the six squares at each timepoint. If you took this approach and decided to sample over three timepoints, here’s what those results might look like.

Soil microbial biomass

By taking the average of all three replicates from each treatment at each timepoint, we can see that the effects of the recommended treatment on microbial biomass were strongest at 6 weeks after application.

How Should I Sample?

  1. Collect composite samples from the top 6 inches of soil with 8-10 cores per sample.
    • If you will be sampling over multiple timepoints, we recommend flagging each spot that composite samples are taken from in order to most accurately compare samples between timepoints.
    • We recommend collecting soil either close to crop roots, where microbes are most abundant, or within the zone of application, where product effects are expected to be strongest.
  2. Fill out the Waypoint Submission Form - example below.
  3. Ship samples to the Waypoint Analytical facility you typically use, or directly to Waypoint, IL (2902 Farber Dr., Champaign IL 61822).
    • DNA is fragile. Store soil samples at room temperature or cooler and make sure to ship soil samples within 3–4 days of sampling. Avoiding shipping samples on Fridays.
    • Like traditional soil samples, soil biology samples can be shipped in paper sampling bags. Soil biology testing will include an S3M test.
Example Soil Sample Info Sheet

What Products Can I Trial With Soil Biology Testing?

Soil biology testing works best for trialing soil-applied products. We do not recommend soil biology testing to trial foliar-applied products. Application methods that involve low product concentrations, such as broadcasting, may also produce subtler effects on soil biology.

Understanding The Report

Example Soil Biology Report

THESE RESULTS, RECOMMENDATIONS AND PREDICTIONS ARE OPINIONS ONLY, DUE TO: (I) THE IMPRACTICABILITY OF OBTAINING FIRST-HAND KNOWLEDGE OF MANY VARIABLE CONDITIONS, (II) THE RELIANCE ON INFERENCES, MEASUREMENTS, AND ASSUMPTIONS WHICH ARE NOT INFALLIBLE, (III) THE PRESENCE OF UNFAVORABLE WEATHER OR GEOLOGIC CONDITIONS, AND/OR (IV) THE NECESSITY OF RELYING ON FACTS, DATA, AND SERVICES FURNISHED BY OTHERS. USER ASSUMES NO OBLIGATION OR LIABILITY FOR THE RECOMMENDATIONS AND PREDICTIONS GIVEN OR RESULTS OBTAINED, AND ALL RESULTS, RECOMMENDATIONS AND PREDICTIONS ARE GIVEN AND ACCEPTED AT SOLE RISK OF THE GROWER. USER EXPRESSLY DISCLAIMS ALL WARRANTIES OR GUARANTEES, EXPRESSED OR IMPLIED, ARISING BY LAW, USAGE OF TRADE, COURSE OF DEALING OR OTHERWISE, RESPECTING ANY RESULTS, RECOMMENDATIONS OR PREDICTIONS, INCLUDING WITHOUT LIMITATION, FITNESS FOR A PARTICULAR PURPOSE, MERCHANT ABILITY OR NON-INFRINGEMENT.

Overall Biofertility

Biology Metric What it measures Functions
Total Microbial Biomass Total DNA content of soil • Source of crop-available nutrients
• Nutrient mineralization
• Residue decomposition
• Shape soil structure
Total Bacteria General abundance of soil bacteria • Decomposition of crop residues and fungi
• Nutrient, carbon cycling
• Soil structure: microaggregate formation
• Higher carbon turnover
Total Fungi General abundance of soil fungi • Residue decomposition
• Nutrient cycling
• Soil structure: macroaggregate formation
• Higher efficiency carbon storage
• Connect distant resources for crops and bacteria

Biofertility: Nitrogen(N)

Biology Metric What it measures Functions
Total N Fixers Native soil bacteria, both “free-living” and symbiotic N fixers, that convert atmospheric N to ammonia N Conversion of atmospheric N to ammonia N
Bradyrhizobia Native soil B. japonicum that nodulate soybean and fix atmospheric N to ammonia N Conversion of atmospheric N to ammonia N for soybean only
Nitrifiers Bacteria and related organisms that convert ammonia N to nitrate N • Conversion of ammonia N to nitrate N
• Necessary for optimal plant uptake, but can contribute to leaching under high moisture conditions or in sandier soils
• Produce nitrous oxide greenhouse gas
Ammonifiers Bacteria that convert nitrate N to ammonia N • Conversion of nitrate N to ammonia N
• Can reduce N losses to leaching by converting to ammonia form
Denitrifiers Bacteria that convert nitrate N to atmospheric N • Conversion of nitrate N to atmospheric N
• Cause significant N losses especially under wet, water-logged conditions
• Produce nitrous oxide greenhouse gas
N2O Reducers Bacteria that convert nitrous oxide N to atmospheric N Mitigate greenhouse gas emissions by reducing nitrous oxide produced during denitrification to atmospheric N
Nitrifier Balance Metric of nitrifying community balance • Describes balance between ammonifier and nitrifier populations
• Higher levels may contribute to conservation of ammonia N under conditions with potential for leaching
• Lower levels may contribute to more available nitrate
N Conservation Potential Metric of overall community balance • Describes nitrogen cycling community balance towards loss or conservation
• Lower values correspond to increased potential for N losses

Biofertility: Phosphorus (P), Potassium (K), and Sulfur (S)

Biology Metric What it measures Functions
Mycorrhizal Fungi Abundance of soil mycorrhizal fungi • Important symbiotic partners of most crops (excluding the mustard family—crops like kale, broccoli, brussels sprouts, etc.)
• Interact directly with crop roots to provide P, water, and other mineral nutrients to crops in exchange for plant sugars
P Mineralization Abundance of bacteria that mineralize organic forms of phosphorus Mineralize P by breaking down organic P forms such as proteins, DNA, phosphate sugars, and phytate
P and K Solubilization Abundance of bacteria that solubilize phosphorus and potassium Production of organic acids that dissolve insoluble forms of P and K
Sulfur Oxidation Abundance of bacteria that oxidize elemental S, producing sulfate Conversion of elemental S to sulfate, the plant-available form of S
Sulfur Reduction Abundance of bacteria that reduce sulfite, producing sulfide • Conversion of sulfite to sulfide
• Cause S losses to the atmosphere (in the form of hydrogen sulfide) or insoluble metal sulfides
• Favored by waterlogged conditions

Soil Biology Case Studies

Location Product App. Method Crop
California Central Valley Plant Nutrition Irrigation Celery
Iowa None None Corn/Soy
Nutrien Ag Solutions Innovation Farm - Kentucky Plant Nutrition None Corn
Nutrien Ag Solutions Innovation Farm - Mississippi None None Cotton
Map of USA Case Studies

California

Central Valley

California Central Valley Results

Plant Nutrition Program to Maximize Yield and Biofertility and Minimize Applied N, P, and K at a Central California Celery Farm

Background

  • A grower split their field between a GSP involving 600 lbs/acre 18-18-18 and a plant nutrition program that greatly reduced N, P, and K inputs
OM pH CEC
1.6% 7.3 24.0

Takeaways

  • Despite lower applied N, P, and K, the plant nutrition program maintained yields at 1,500 cartons/acre
  • The plant nutrition program increased most markers, but especially overall microbial biomass, P mineralizers, and P & K solubilizers
    • Higher microbial biomass should improve nutrient mineralization and soil structure
    • P mineralization and P and K solubilization make inaccessible P and K, like the P and K in residues, available to crops

Iowa

Topography can drive patterns in soil biology

Topography Can Drive Patterns in Soil Biology

Background

  • A field in Iowa was grid sampled for soil biology testing
OM pH CEC TEXTURE
3.7% 6.6 14.9 Loam; Sandy loam

Takeaways

  • Microbial biomass metrics are all highest in low-lying portions of the field
    • Rainfall and erosion can cause applied nutrients and topsoil to collect in low-lying areas
  • Careful consideration of factors like topography is needed when deciding where to take soil biology samples, especially when those samples are being used to build field-level recommendations
    • The usefulness of biocatalyst recommendations, which are made under overall low levels of soil biology, may change if samples are pulled exclusively from especially low- or high-elevation areas

Kentucky

Nutrien AG Solutions Innovation Farm

Kentucky results

Plant Nutrition Program Improves the Abundance of P- And K- Cycling Microbes for Months After Treatment

Background

  • Nutrien Ag Solutions Innovation Farm in Hopkinsville, KY has been applying 300 lbs/acre of 9-23-30 with or without an added plant nutrition product to corn pre-plant for 5 years
OM pH CEC TEXTURE
2.8% 5.8 8.4 Silt loam

Takeaways

  • This year, 1 month after application, a plant nutrition program increased available P by 36%, but had not yet changed soil biology markers
  • At both 2 and 3 months after a plant nutrition application, even though available P levels became similar between a plant nutrition program and GSP fields, P-cycling markers were higher
    • Both P mineralizers and P and K solubilizers create plant available P and K from organic and inorganic sources that crops cannot tap into themselves

Mississippi

Nutrien AG Solutions Innovation Farm

Mississippi results

Rotating Cotton With Corn or Soy More Than Doubles Microbial Populations and Builds up Soil Organic Matter

Background

  • At the Nutrien Ag Solutions Innovation Farm in Winterville, MS, three cotton fields have been rotated with corn or soy, while another four fields are continuous cotton
  • All fields were in cotton in 2023
  • Corn-cotton and corn-soy rotations can help introduce more nitrogen-rich corn and soy residue into the soil. These nitrogen-rich residues are more desirable food for microbes than the woody, nitrogen-poor cotton residues
OM pH CEC TEXTURE
1.3% 6.3 10.9 Very fine sandy loam

Takeaways

  • Compared to the continuous cotton fields, the three fields in cotton-corn or cotton-soy rotations had more than double the soil bacteria, fungi, and overall microbial biomass
    • All that additional microbial biomass increases the soil’s pool of mineralizable nutrients
  • Fields in cotton-corn and cotton-soy rotations also had more organic matter
    • Organic matter is strongly correlated with microbial biomass
  • Management changes can have big consequences for soil biology

Contact

If you would like more information on soil biology testing, including how to submit samples, use soil biology testing in trialing, or interpret results, reach out to your Waypoint Sales Team Representative.

If you have questions about the report or your sample results, please contact: Emily Tronson, ETronson@waypointanalytical.com or Alicia Bryan ABryan@waypointanalytical.com

Waypoint Sales Team

Bill Young, National Sales
BYoung@waypointanalytical.com

Louie Garrison, National Customer Support
LGarrison@waypointanalytical.com

Oscar Ruiz, National Sales Support
ORuiz@waypointanalytical.com


Alicia Bryan, Soil Biology Sales
ABryan@waypointanalytical.com

Lizzie French, Soil Biology Manager
LFrench@waypointanalytical.com

Emily Tronson, Soil Biologist
ETronson@waypointanalytical.com


Joe Thelen, Midwest / Cornbelt / Great Plains
JThelen@waypointanalytical.com

Alan Meijer, East
AMeijer@waypointanalytical.com

Michael Goedeken, Great Plains / Cornbelt
MGoedeken@waypointanalytical.com

Downloadable PDF

A pdf is available for download if you wish to have a downloadable version of this article.

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