Equipment
Clean soil probe or appropriate sampling tool, clean non-reactive bucket, labeled laboratory bag or container, location map, and field record. Avoid tools or containers that could contaminate the requested analysis.
Methods that show their work
These guides help structure field records. They are screening and sampling workflows, not substitutes for crop-specific laboratory instructions, local calibration, safety requirements, or professional advice.
Method 01
The laboratory analyzes the submitted soil—not the whole field. Sampling design determines what area the result can reasonably represent.
Use the depth, timing, container, and handling instructions specified by the laboratory and the locally calibrated recommendation system for your crop.
Clean soil probe or appropriate sampling tool, clean non-reactive bucket, labeled laboratory bag or container, location map, and field record. Avoid tools or containers that could contaminate the requested analysis.
A composite describes an average of the included material and can hide important spatial variation. University of Minnesota Extension gives 15–30 subsamples and a 0–6 inch depth as one crop- and system-specific example; use local instructions rather than treating those numbers as universal.
Reference: UMN Extension soil sampling guidance →Method 02
Measure how quickly a defined depth of water enters the soil under a recorded field condition. The result is sensitive to soil moisture, cracks, surface cover, ring installation, and water head.
Recent rain or irrigation, starting moisture, surface residue, crusting, slope, vegetation, soil temperature if relevant, ring diameter, insertion depth, and whether a single- or double-ring method is used.
A field ring test is useful for screening differences and monitoring a defined location. It is not automatically saturated hydraulic conductivity, and one placement cannot characterize an entire field.
Reference: USDA NRCS Soil Quality Test Kit Guide →Method 03
Observe how an air-dry soil aggregate holds together when immersed. The test illustrates stability under a specified procedure; it does not measure every cause of aggregation.
Slaking—the breakdown of an aggregate during rapid wetting—is not the same as clay dispersion. The NRCS field method specifies air-dry aggregates and a defined observation sequence.
Reference: USDA NRCS Soil Survey Field and Laboratory Methods Manual →Method 04
A penetrometer can help locate resistant layers, but readings change strongly with soil moisture, texture, stones, roots, operator speed, and equipment.
Use resistance patterns alongside moisture, rooting, structure, bulk density if available, and known traffic history. A high reading may flag where to investigate; it does not by itself establish cause or crop response.
Reference: USDA NRCS Cropland In-Field Soil Health Assessment Guide →Method 05
Tissue interpretation depends on the crop, growth stage, plant part, sampling position, handling, and reference population used by the laboratory.
Obtain the receiving laboratory’s current instructions for crop, growth stage, plant part, sample count, cleanliness, packaging, and shipping. Record foliar products, dust, disease, water stress, and recent weather that could affect the sample.
Plan the comparison
OpenSoil’s field-record tools will preserve raw observations, methods, timing, units, and changes—not just a final score.