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Soil Vitality Index (SVI)
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Soil Vitality Index (SVI)

A Qualitative Framework for Assessing Soil Biological Vitality

1. Introduction

The Soil Vitality Index (SVI) is a microscopy-only, qualitative framework for evaluating the biological vitality of soils. Inspired by Index-of-Biological-Integrity (IBI) logic from aquatic ecology, it links what is seen under the microscope to  clear, image-based scoring levels. The aim is to deliver a method that is reproducible, comparable over time and space, and practical for trained technicians.

2. Challenges in Soil Health Assessment

Soil health is the capacity of soil to function as a living system. Physical and chemical conditions set the stage; the biological community drives decomposition, nutrient cycling, aggregation, gas and water regulation, and plant resilience. In practice, soil health is largely microbial: without an active, balanced community, soils cannot reliably provide these services.

Microscopy has helped show that soil function emerges from biological networks interacting with physics and chemistry. Vitality depends on diversity, connectivity, and sustained activity. Yet, microscopy faces limits:

These issues call for a qualitative, multi-metric approach that synthesizes indicators into a clear score.

3. The Soil Vitality Index Approach

The SVI turns visual evidence into scores (0/1/3/5) using image-based levels and basic quality checks. It improves comparability and practicality without relying on exact counts, staying accessible to trained technicians.

General note: See Appendices 1–5 for detailed protocols and scoring guidance

3.1. What we score

These six metrics reflect key food web functions visible under microscopy, detailed in Appendix 3.

Each is scored 0/1/3/5, summed (030), and mapped to a qualitative class for reporting. Clear examples for each level reduce subjectivity.

3.2. Benefits

Focusing on a few visual indicators and levels cuts variability between analysts, avoids false precision, and keeps the method teachable. Results suit comparisons and trends (same plot, season, protocol) over species-level details. Visual thresholds, calibrated regionally, ensure consistent abundance assessments across variable samples.

4. Intrinsic limits (and how SVI manages them)

Mitigation: Emphasize function, avoid species claims.

Mitigation: Use image guides, minimum views, and double-checks. Training with inter-technician photo reviews enhances consistency.

Mitigation: Standard sampling, handling rules, time limits.

Mitigation: Set equipment standards and protocols.

Mitigation: Compare like-with-like and track trends.

Mitigation: Use replication for change detection.

Mitigation: Build local baselines and refine levels.

Mitigation: Pair with physical/chemical data.

These limits are managed through standardized methods, ensuring results are for trends, not absolutes.

 

5. Applications

The SVI is a practical soil-only tool that adds a consistent biological view to complement physical and chemical tests. It supports decision-making, not species diagnostics.

5.1. Well-suited uses

The SVI excels at comparisons and trends.

5.2. Out of scope / deliberately not provided

6. Method Overview

The SVI uses six metrics, scored 0 to 5 based on visual thresholds, totaling 0 to 30, then mapped to:


7. Next Steps

The draft will be shared with practitioners and researchers for review across contexts. Feedback will refine levels, scoring, and robustness. Priorities include clear technician guides, a scorecard with photo examples, and inter-lab calibration. Calibration notes and photo-based scorecards will be shared publicly post-review to support local application.

8. Governance & Versioning

The Soil Vitality Index is being developed as a collective effort. At this early stage, this document reflects the consensus of the founding contributors.

This section will be expanded in the next version to describe the full process for updates, calibration integration, and community review.

Change Log

v0.1 – August 2025: Internal draft circulated among founding contributors.


Appendices

Appendix 1 - Sampling Protocol

Appendix 2 - Analysis Protocol

Appendix 3 - Scoring Parameters

Appendix 4 - Calibration protocol


Appendix 1 - Sampling Protocol

  1. Optimized Consistency
  1. Systematic Recording of External Variables
  1. Field sampling guide ( the W-walk)
  1. Post-Sampling Handling

Appendix 2 - Analysis Protocol

  1. Sample preparation (setting up a microscope slide)
  1. Microscope and camera setup
  1. Sample analysis

Appendix 3 - Scoring parameters

Each metric is scored 0, 1, 3, or 5 based on microscopic observation (100x–400x magnification) following adapted SFW protocols. Six metrics yield a total score (0–30), then translated into a qualitative rating. All parameters used in the table below are illustrative, as the actual parameters to be used are only available in the regions which have already been calibrated.

Metric

Score 5

Score 3

Score 1

Score 0

Bacterial Diversity

>10 morphotypes

5–10 morphotypes

1–4 morphotypes

None visible

Bacterial Abundance

Dense, most fields

Moderate, several fields

Sparse, few fields

None

Fungal Diversity

>5 filament types

2–5 filament types

1 type

None

Fungal Abundance

Dense network, most fields

Moderate, several fields

Sparse, few fields

None

Protozoan Diversity

≥3 active types

2 types

1 type

None

Trophic Interactions (protozoa + nematodes)

Protozoa + ≥2 beneficial nematode guilds

Protozoa + 1 guild

Protozoa only

None

Methodological Notes


Appendix 4 – Calibration Protocol

The Soil Vitality Index (SVI) is not intended to produce universal scores that can be compared across countries or climates. Instead, calibration is carried out per geographical region to ensure that the scoring reflects what is realistically achievable under local conditions. The key is to define what “maximum potential vitality” looks like for the soil types present in that region.

1. Purpose of Calibration

2. Calibration Process

  1. Score all samples using the standard SVI rubric.

  2. Group results by soil type (sandy, loamy, clayey).

  3. Within each soil type, examine the distribution of scores from the exemplary farms.

  4. Set the “Highly Vital” threshold for that soil type so that the best farms fall within the 21–30 range. If most exemplary parcels in a given soil type fail to reach “Highly Vital,” adjust the visual descriptors (e.g., what qualifies as “dense coverage”) to better reflect the maximum potential for that soil type.

  5. Publish a short calibration note for the region: “In loamy soils, Highly Vital corresponds to [X visual conditions]; in sandy soils, to [Y conditions], etc.”

Example Calibration Table (Illustrative)

Metric

Sandy soils (low organic retention)

Loamy soils (balanced texture)

Clayey soils (high surface area, high potential)

Bacterial abundance

“Dense” = frequent but patchy coverage in ~30–50% of fields of view

“Dense” = uniform coverage in ~60–70% of fields

“Dense” = nearly all fields thick with bacteria; activity obvious

Bacterial diversity

“High” = 6–8 distinct morphotypes

“High” = 8–10 morphotypes

“High” = >10 morphotypes commonly observed

Fungal abundance

“Dense” = hyphae visible in many fields, but not continuous networks

“Dense” = clear hyphal networks spanning fields

“Dense” = thick, branching networks across most fields

Fungal diversity

“High” = ≥2 filament types

“High” = 3–4 filament types

“High” = ≥5 filament types (varied diameters, textures)

Protozoan diversity

“High” = ≥2 active types (usually flagellates + amoebae)

“High” = ≥3 active types

“High” = ≥3 active types, abundant across fields

Trophic interactions

Protozoa + at least one beneficial nematode guild occasionally present

Protozoa + ≥1 nematode guild consistently present

Protozoa + ≥2 nematode guilds often visible

How to Use This Table