Saturated paste and ammonium acetate mineral analysis, Logan Labs · Sample garden: raised beds, Marin County · organic · municipal water · sampled 0–6 in.
Sample data from a representative Bay Area garden. Your report is built the same way from your own lab numbers.
Hillside dig red
PAGE 1
Your Soil in One Page
This is a well fed but badly balanced garden soil, a pattern that can follow years of generous compost and manure. There is plenty of organic matter and a large phosphorus bank, but the two tests agree that potassium and boron are short. Magnesium is taking more than its share of the soil’s holding sites while calcium is short both in the bank and in the water roots drink from. The job is not to pile on more of everything. It is to move the balance.
Soil Score · Cure Soil field guide
23/100
Well fed, badly balanced.
This score counts the measured flags in the saturated paste for 62.5% and in the mineral reserve for 37.5%, because there is no biology test here. When biology is tested, the weights are paste 50%, mineral 30% and biology 20%. Priority findings carry an extra penalty. It is our field guide for comparing rounds, not a certified lab grade. A single number never replaces the lab results and the reasons below.
Read honestly
Potassium is short on both tests. The saturated paste reads 5.9 ppm against a 12–15 ppm guide, while the mineral report shows 306 lbs/ac found against 437 desired, a 131 lbs/ac deficit. When two methods agree, it is a real shortage, not a single bad sample.
Calcium sits below the Albrecht band. Calcium fills 58% of the holding sites against the 60–70% band, and the paste reads 22 ppm against 25–30. Calcium and magnesium compete for those sites; simply adding more fertilizer without rebalancing leaves roots short.
Magnesium is crowding both lenses. The mineral read finds 19% saturation against the 15% point, while magnesium makes up 34.5% of the dissolved base cations. Leave Epsom salt and dolomite out so you do not push calcium further back.
Boron is short in the paste and the bank. Paste boron is 0.04 ppm against 0.08; the mineral read is 0.45 ppm against 0.7. Boron supports new growth and flower set, but it becomes toxic quickly, so any correction must be divided into small applications.
Sodium needs a water check. Sodium in the paste is 6.2 ppm and 11.6% of the dissolved cations. It is over the 4–5 ppm ceiling. Municipal water may be adding it each time you irrigate; test the water rather than assuming the source.
The phosphorus bank is already large. The mineral report shows 640 lbs/ac, 3.2× the 200 lbs/ac reference. More phosphorus can tie up the micronutrients plants need, and Christine Jones found it suppresses the mycorrhizal fungi that would unlock this bank.
Where your soil is working
Organic matter gives soil life fuel. The mineral test shows 5.8% organic matter. That is food and habitat for the soil food web, although it does not measure the organisms themselves; only a separate biology test could do that.
The root zone solution is low in salt. Soluble salts read 180 ppm and chloride 14 ppm. Those readings mean roots are not currently fighting a salty solution to take up water.
pH is comfortable for vegetables. The mineral pH is 6.6 and the paste pH is 6.8. At this level, roots can reach many nutrients already in the soil; adding lime would push it higher for no good reason.
Iron and aluminum are behaving. Paste iron reads 1.1 ppm and aluminum 3.2 ppm. These do not call for a product on their own; the reserve is available, while the dissolved aluminum is not dominating the root zone water.
Bottom line: Feed the measured potassium and boron shortages, bring calcium back into balance, and stop feeding the phosphorus and magnesium this soil already owns. Keep compost, extract and living roots working so the mineral bank becomes food the plant can actually reach. Retest before calling it fixed.
PAGE 2
The Plan
Each line starts with the two lab tests, then the action. The default amounts are for 100 square feet of garden; switch to farm scale for acres. A rate only makes sense when it is sized to the shortage, split so roots can use it, and checked against the next report.
Rate view
Potassium · first priority
Do this. Use organic sulfate of potash (SOP 0-0-50), sized to the printed 131 lbs/ac deficit. About 0.72 lb (11.5 oz) of product per 100 sq ft for the season; split into 4 watered in applications of about 3 oz.
Why. Both tests agree: paste potassium is 5.9 ppm against 12–15, and the mineral bank holds only 70% of the desired amount. Potassium moves water and sugar through a plant and helps fruit fill.
If you skip or overdo it. Leave it short and the plant struggles to move water and fill fruit; put it all on at once and the root zone gets a salt spike.
How to tell it worked. Next round, paste potassium should move toward 12–15 ppm, with a smaller exchange deficit.
Calcium · Albrecht correction
Do this. Use gypsum, not lime, because calcium saturation is moderately low at 58%, exchange calcium is at 85% of desired, and pH is already 6.6. About 5.5 lb gypsum per 100 sq ft for the season, split into 2–3 applications.
Why. Gypsum supplies calcium without raising pH. Calcium and magnesium compete for the same holding sites, so raising calcium’s share helps push excess magnesium down. Gypsum’s sulfate also supports the low sulfur (mineral 18 vs 25 ppm; paste 3.1 vs 5.0 ppm), so do not add separate sulfur.
If you skip or overdo it. Skip the correction and magnesium keeps crowding calcium; use lime instead and pH rises unnecessarily.
How to tell it worked. Next round, calcium saturation should move toward the 60–70% band and paste calcium toward 25–30 ppm.
Boron · gently
Do this. Dissolve about 5 g Solubor per 100 sq ft for the season in water and split it into 4 applications. About 5 g Solubor per 100 sq ft total across 4 watered in applications.
Why. Paste boron is 0.04 ppm and mineral boron 0.45 ppm, both below target. Boron supports new growth and flowering, but the gap between enough and too much is narrow.
If you skip or overdo it. Leave a real shortage and new growth can struggle; apply it all at once and boron can burn leaves.
How to tell it worked. Next round, both boron readings should improve without leaf edge burn.
If calcium had been severely low (saturation under 55% or less than 60% of the desired exchange calcium), this plan would call for Eden soluble calcium instead, with its rate set by Cure Soil. This garden is moderately low, not severe, so gypsum fits the report.
None, and why
Phosphorus. None, because the reserve is 3.2× the reference at 640 lbs/ac. Added phosphorus ties up micronutrients and suppresses the mycorrhizal fungi that unlock what is already there.
Magnesium. None, because exchange magnesium is at 158% of desired. Epsom salt and dolomite both add more magnesium and crowd out calcium.
Nitrogen. None separately, because this organic soil has 5.8% organic matter and the soil food web releases nitrogen as it works. Only a measured trigger would change that decision.
Zinc. None, because mineral zinc is 22 ppm, already above the 5–10 ppm range. Extra zinc can press on iron and phosphorus.
Iron. None, because the mineral bank holds 180 ppm and paste iron is 1.1 ppm. There is no shortage to fix.
Manganese and copper. None yet. Both read low in soil and paste, but test the plant tissue before adding anything. Compost biology and fermented humic acid may mobilize what the soil already owns; a guess can overshoot.
Always on
On open beds, top dress Cure Soil compost, water it in within a day and follow with fresh living extract. Elaine Ingham showed that the organisms in the soil food web release nutrients as they feed on each other: biology is how the mineral bank gets spent. Fermented humic acid helps hold minerals in plant reachable forms and feeds fungi. If you skip the biology, a soil can own plenty and still leave roots hungry.
Before extract goes through a hose, check municipal water for free chlorine and sodium. Free chlorine must read zero at the hose end, or it kills the extract you paid to make; sodium brought by irrigation can build up week after week.
For an organic site, check each input against your certifier’s approved list before applying it. Document a tissue confirmed deficiency before spraying micronutrients, or you risk both a needless dose and a certification problem.
PAGE 3
How to Read This Report
Two lenses, one sample. Saturated paste is a lab test that wets soil to saturation, squeezes out the water and measures the minerals dissolved in it. That is the closest a soil test gets to asking what roots can drink this week. Ammonium acetate extraction measures the minerals held on the soil particles: what this soil owns in the bank and can trade into the water over time. Read both before buying a product, because a low paste number can sit beside a full bank.
Why ammonium acetate? It measures the exchangeable base cations (positively charged minerals like calcium, magnesium, potassium and sodium) against this soil’s holding capacity. Mehlich III phosphorus is a separate reserve number printed with the mineral report, not a substitute for the exchange test. Comparing results from unlike extraction methods as though they were the same test produces a false trend.
Flags are clues, not prescriptions. A gold ▼ means below the shown target, ▲ means above it, ● means inside the band and — means there is no target or nothing printed. One flag says where to look; a recommendation requires the paste, the mineral bank and the whole garden context together. A value below detection stays printed as “less than,” never as zero.
Base saturation is the share of the seats. Total exchange capacity (TEC) is how many nutrient holding sites this soil has. Calcium, magnesium, potassium and sodium compete for those same sites. William Albrecht aimed for calcium near 65%, with 60–70% as the useful band, magnesium near 15%, potassium near 3.5% and sodium low. If magnesium takes too many seats, roots can run short of calcium even in well fed soil.
Desired amounts scale to this soil. A desired amount is the lab’s estimate for this garden’s TEC, not a universal dose. “Found versus desired” shows the gap. A product rate still depends on the crop, the paste, the pH and what else the product adds.
Depth stays fixed. This sample is from 0–6 inches, a depth factor of 2.0 in the mineral calculation. On the next round, take cores from the same spots and the same depth; otherwise a changed number might be a changed sample, not changed soil.
PAGE 4
Saturated Paste · What the Roots Can Drink
This is the primary lens. Every row describes what is dissolved in the water around the roots right now. A low dissolved number may be a true shortage or a mineral stranded in the bank; page 5 tells the difference.
Parameter
Target
Your soil
Flag
What it means
pH
Context only
6.8
—
This measures acidity. In a comfortable range, vegetables can reach more of the nutrients already present.
Soluble salts
Context only
180 ppm
—
This is dissolved salt in the root zone water. Too much salt makes roots work harder to drink.
Chloride
Context only
14 ppm
—
Chloride comes in with salts and water. Keep an eye on it, especially with sensitive crops.
Bicarbonate
Context only
55 ppm
—
Bicarbonate in irrigation water can lock up calcium. A paste reading alone does not replace a water test.
Sulfur
5
3.1 ppm
▼
Sulfur is needed for plant proteins. Read it alongside the exchange reserve so a low paste number does not trigger a needless extra product. The value is below the guide; check the mineral bank before adding any sulfur.
Phosphorus
0.4
0.9 ppm
▲
Phosphorus supports root growth and flowering. A high reserve can still coexist with a small dissolved amount, so read both lenses. The value is above the guide; avoid adding more until the next test shows it has come down.
Calcium
25–30
22 ppm
▼
Calcium builds firm cell walls and soil crumbs. Compare this week’s dissolved amount with the mineral reserve before adding a product. The value is below the guide; check the mineral bank before adding any calcium.
Magnesium
5–6
9.6 ppm
▲
Magnesium supports chlorophyll, but too much in solution crowds out calcium. The value is above the guide; avoid adding more until the next test shows it has come down.
Potassium
12–15
5.9 ppm
▼
Potassium moves water and sugars through a plant and helps fruit fill. A low paste reading means roots cannot drink enough this week. The value is below the guide; check the mineral bank before adding any potassium.
Sodium
0–5
6.2 ppm
▲
Sodium competes with the useful bases. When it is high in solution, check what irrigation water brings. The value is above the guide; avoid adding more until the next test shows it has come down.
Boron
0.08
0.04 ppm
▼
Boron supports new growth and flower set. Plants need very little, and the gap between enough and too much is narrow. The value is below the guide; check the mineral bank before adding any boron.
Iron
0.5–3
1.1 ppm
●
Iron helps leaves make chlorophyll. Check the reserve and the leaf before buying any iron.
Manganese
0.1–0.25
0.06 ppm
▼
Manganese helps with photosynthesis. A low solution number alone is not permission to apply it; confirm a shortage in plant tissue. The value is below the guide; check the mineral bank before adding any manganese.
Copper
0.07
0.03 ppm
▼
Copper helps enzymes work. Soil and paste numbers guide the question, but tissue evidence is needed before any spray. The value is below the guide; check the mineral bank before adding any copper.
Zinc
0.1
0.18 ppm
▲
Zinc helps growing tips. If the reserve is already ample, a low paste reading calls for biology before another input. The value is above the guide; avoid adding more until the next test shows it has come down.
Aluminum
0–10
3.2 ppm
●
Aluminum can stress roots when it becomes soluble. A low dissolved value here is good news.
What the paste is saying. The water around these roots is low in salt but not balanced. Potassium is at 5.9 ppm versus 12–15, calcium is at 22 versus 25–30, boron is at 0.04 versus 0.08, and magnesium takes 34.5% of the dissolved base cations. The soil is not starving everywhere; it is spending unevenly. Page 5 shows whether those shortages are real holes in the bank or only slow withdrawals.
PAGE 5
Ammonium Acetate · The Soil's Bank
This test reads the reserve held on mineral and organic surfaces. “Found” and “desired” are scaled to this soil’s total exchange capacity, not a blanket fertilizer recipe. When a reserve and the paste tell the same story, the case for action gets stronger.
Parameter
Target
Found vs desired
Saturation
Flag
What it means
Total exchange capacity (TEC)
Context only
14 M.E.
—
—
Total exchange capacity (TEC) tells us how many nutrient holding sites this soil has. Desired mineral amounts scale to this capacity.
pH
Context only
6.6
—
—
This measures acidity. In a comfortable range, vegetables can reach more of the nutrients already present.
Organic matter
Context only
5.8%
—
—
Organic matter feeds soil organisms and helps soil hold water. It does not tell us by itself how active the biology is.
Sulfur
25
18 ppm
—
▼
Sulfur is needed for plant proteins. Read it alongside the exchange reserve so a low paste number does not trigger a needless extra product. This reserve is short against the guide, so confirm with the paste before setting a dose.
Mehlich III phosphorus (P₂O₅)
200 lbs/ac
640 lbs/ac
—
—
This is the phosphorus bank measured by a different extraction within the mineral report. A large bank is a reason not to add more.
Calcium
65% saturation (band 60–70%)
1624 ppm = 3248 lbs/ac found / 3808 lbs/ac desired (85% of desired)
58%
▼
Calcium builds firm cell walls and soil crumbs. Compare this week’s dissolved amount with the mineral reserve before adding a product. This reserve is short against the guide, so confirm with the paste before setting a dose.
Magnesium
15% saturation (band 10–20%)
319 ppm = 638 lbs/ac found / 403 lbs/ac desired (158% of desired)
19%
●
Magnesium supports chlorophyll, but too much in solution crowds out calcium.
Potassium
3.5% saturation (band 2–5%)
153 ppm = 306 lbs/ac found / 437 lbs/ac desired (70% of desired)
2.8%
●
Potassium moves water and sugars through a plant and helps fruit fill. A low paste reading means roots cannot drink enough this week.
Sodium
0–0.5% target; band 0.5–3%
39 ppm = 77 lbs/ac
1.2%
●
Sodium competes with the useful bases. When it is high in solution, check what irrigation water brings.
Other bases + hydrogen
Context only
19%
—
—
These occupy the remaining holding sites. All saturation shares together describe the soil’s mineral balance.
Boron
0.7
0.45 ppm
—
▼
Boron supports new growth and flower set. Plants need very little, and the gap between enough and too much is narrow. This reserve is short against the guide, so confirm with the paste before setting a dose.
Iron
Context only
180 ppm
—
—
Iron helps leaves make chlorophyll. Check the reserve and the leaf before buying any iron.
Manganese
Context only
35 ppm
—
—
Manganese helps with photosynthesis. A low solution number alone is not permission to apply it; confirm a shortage in plant tissue.
Copper
Context only
2.4 ppm
—
—
Copper helps enzymes work. Soil and paste numbers guide the question, but tissue evidence is needed before any spray.
Zinc
5–10 ppm
22 ppm
—
—
Zinc helps growing tips. If the reserve is already ample, a low paste reading calls for biology before another input.
Aluminum
Context only
850 ppm
—
—
Aluminum can stress roots when it becomes soluble. A low dissolved value here is good news.
Where the two tests agree. Potassium and boron are short in the solution and the bank. Calcium is below the Albrecht saturation band and low in the paste. Magnesium is high on the holding sites and takes too big a share of the dissolved cations. That convergence, rather than any one arrow in a table, is why the plan feeds potassium and boron, rebalances calcium, and leaves magnesium alone.
PAGE 6
Soil Story, Mulder’s Chart and Next Round
This garden has been loved hard. Years of compost and manure left it with 5.8% organic matter and a phosphorus bank 3.2 times the guide. That is a real asset, but it is not permission to keep feeding everything. Too much phosphorus can tie up the little minerals a plant needs to defend itself.
Under that full pantry, potassium is short where roots drink (5.9 ppm against 12–15) and in the reserve (306 versus 437 lbs/ac desired). Boron is thin in both places too. Magnesium takes 19% of the holding sites while calcium only holds 58%, below William Albrecht’s 60–70% band. The water roots drink tells the same story: there is too much dissolved magnesium relative to calcium.
So the move is precise, not loud. Feed the measured potassium shortage in small splits, correct calcium with the right carrier for this pH and sulfur read, and nudge boron gently. Leave phosphorus, magnesium and extra nitrogen alone. Keep living compost, fresh extract and fermented humic acid working: the organisms are how a stocked bank becomes food in the root zone.
Then come back to the same spots. If potassium, calcium and boron move toward their guides without salt or other excesses climbing, the garden is finding its balance. If they do not, we read the next numbers and change course. That is how we treat the soil, not the symptoms™.
Mulder’s chart
William Albrecht taught that nutrients compete for space on the soil’s holding sites. In this ring, solid lines mark nutrients an excess can press down, while dashed lines mark helpful relationships. Only lines from excesses in this soil are lit. High phosphorus presses on calcium, potassium, copper and iron; high magnesium presses on iron; and high zinc presses on iron and phosphorus. That is why fixing calcium and potassium together makes more sense than chasing every low number with another bottle.
Next round
Retest three anchor numbers from the same spots and the same 0–6 inch depth in 6–12 months. That keeps the lab method and sampling depth steady, so a change in the numbers is a change in the soil rather than a change in where you dug.
01
Paste potassium · now 5.9 ppm, moving toward 12–15.
02
Calcium saturation · now 58%, moving toward 60–70%.