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Montmorillonite Clay (this product)
Dr Forest Mineral Mix
Customer highlight
The best clay mineral mix Ive found, as with all Dr Forest products I highly recommend them for organic growers.
Editorial highlight from marketplace and store reviews — separate from the full review list below.
Montmorillonite clay is a natural swelling clay mineral from bentonite deposits that adds cation exchange capacity (CEC) to soils and growing media that have almost none. Its plate-like layers carry a negative charge, so they hold calcium, magnesium, potassium and ammonium against leaching and hand them back to roots as the soil solution is drawn down. Water sits between the same layers and is released as the medium dries. Dr Forest supplies it as fine grey-green granules, packed in small batches in Stockport, Greater Manchester, with nothing added.
It is for sandy soils, peat-free composts and any container mix that drains well but holds on to nothing. Being a mineral, it does not rot down or wear out: what you add this spring is still working in ten years. Pack sizes run from 1.5 kg to 15 kg, and the bigger packs cost less per kilo.
Weighed and packed in small batches at our workshop in Stockport, Greater Manchester. A mined mineral, unprocessed and vegan, with nothing added. It sits alongside the rest of our soil improvers; for where clay fits in a mineral programme, read what are organic dry amendments? Made by Growers. Backed by Science.
Montmorillonite is a 2:1 phyllosilicate. Each layer is an aluminium octahedral sheet sandwiched between two silica tetrahedral sheets, and the layers stack with a gap between them (the interlayer) that water and cations can enter [1]. Substitutions inside the sheets leave the layers with a permanent negative charge, which is what attracts and holds positively charged nutrient ions. Bentonite is the rock; montmorillonite is the mineral that makes up most of it, and that is what is in the bag.
Because the interlayer surfaces count as well as the outside of each particle, the total surface area is estimated at 700–800 m² per gram [1], which is why a small dose does a lot of work. The same structure is why it swells: water moves between the layers and is held there until the surrounding medium dries and pulls it back. The calcium form expands far less in water than the sodium form [8]; the FAQ covers which form this is. Humic substances bind to those same surfaces, the mechanism behind clay-humus complexes; see what is humic acid? for the other half of that partnership.
| Mineral | CEC (meq per 100 g) | Swells in water |
|---|---|---|
| Kaolinite | 3–15 | No |
| Illite | 10–40 | Very little |
| Montmorillonite | 70–100 (Carroll); 80–150 (Jemai et al.) | Yes |
| Vermiculite | 100–150 | Limited |
Figures from Jemai et al. (2024) and Carroll (1959) [1, 2]. Montmorillonite holds roughly five to thirty times more exchangeable cations per gram than kaolinite, a common clay in garden soils. It is not the highest of all minerals; vermiculite edges it. What montmorillonite offers is high CEC, reversible swelling and a price that makes sense by the kilo. Sand contributes almost no exchange capacity at all, which is why sandy soils need feeding so often.
Negatively charged clay surfaces hold Ca²⁺, Mg²⁺, K⁺ and NH₄⁺. When a root takes up nutrients it releases H⁺, which displaces a stored cation from the clay for the root to absorb. In a column study on sandy soil, Hussain et al. (2022, PLOS ONE) found that bentonite at 2–4% cut nitrate in the leachate by 12–19% across three nitrogen sources, and by 20–25% at the 4% rate with calcium nitrate [3]. Less in the drain, more in the soil.
Mi et al. (2020, Scientific Reports) applied bentonite once, at 6–30 tonnes per hectare, to a sandy loam in northern China and followed it for five seasons. Field water-holding capacity and plant-available water in the top 40 cm were significantly higher throughout, and millet grain protein rose by up to 28% over the control [4]. One application, five years of measurable effect.
Farghali and Tammam (2026, BMC Plant Biology) grew maize and senna in three desert sandy soils amended with 1.5%, 3% and 5% bentonite by weight. Soil water content, shoot length, root length, chlorophyll and fresh weight all improved over the unamended control [5]. Garden rates are lower than this, but the direction matches the field trials above.
Protein-rich material breaks down to ammonium, and in a heap with nowhere to hold it, ammonium leaves as ammonia gas. That is the smell, and it is nitrogen lost. Li et al. (2012, Bioresource Technology) composted pig manure with bentonite and found it sped up organic matter breakdown and raised the total nitrogen of the finished compost; they recommend keeping bentonite under 2.5% of the mix [6]. A few handfuls per barrowload is well inside that.
Six et al. (2002, Plant and Soil) identified close association with silt and clay particles as one of three main routes by which soil carbon is protected from microbial breakdown [7]. A sandy soil has few of those surfaces, so compost added to it disappears quickly. Add clay and the organic matter has somewhere to bind and stay.
Field studies above used agricultural rates on bare sandy soils. They describe the mechanism; the effect at garden rates will be smaller.
A tablespoon is approximately 12–15 g of clay. Soil-mix rates are given in millilitres per litre of medium; bed and lawn rates in grams per square metre.
Fertilisers and biological amendments are used up and need replacing. Montmorillonite is a mineral that does not degrade. Once mixed into soil or growing media it stays there, holding nutrients, absorbing water and supporting structure indefinitely. Each application is a permanent upgrade to the medium. In containers, that is also the reason to stick to the rates: do not exceed 5 ml per litre, because too much clay in a confined volume can impede drainage.
Mix thoroughly into potting compost, peat-free media or living soil blends before planting. Even at the lower rate (2.5 ml/L) the CEC improvement is significant: the 800 m²/g surface area means a small amount of clay contributes an enormous number of exchange sites. Use the higher rate (5 ml/L) for very sandy or fibre-based media with minimal native CEC. Do not exceed 5 ml/L in container mixes. Too much clay can impede drainage in confined volumes.
Sprinkle over the soil surface and water in well. The clay particles work into the soil profile over successive waterings. Top dressing is for existing plantings where you cannot remix the soil; the clay incorporates gradually from the surface down. Use the lower rate for maintenance on media that already contain some clay, and the higher rate for very free-draining media that are losing nutrients rapidly. There is a method piece on how to top dress if you are new to it.
Scatter over the soil surface and fork or rake into the top 10–15 cm. Water in well. Use the higher rate (300–500 g/m²) for sandy and free-draining soils that are losing nutrients and drying out rapidly. Use the lower rate (100–200 g/m²) as annual maintenance on soils that have been previously amended. The effect is cumulative and permanent: each application adds to the CEC reservoir that remains in the soil indefinitely.
Sprinkle montmorillonite between layers of compost material, particularly when adding high-nitrogen materials (grass clippings, kitchen waste, manure) that tend to produce ammonia. The clay captures ammonium ions before they volatilise, retaining nitrogen in the compost and reducing odour. The finished compost will have a higher nitrogen content and a richer mineral profile than compost made without clay.
Broadcast over the lawn after scarifying or aerating. The clay particles need to reach the root zone, so application to recently aerated turf is far more effective than scattering on a dense, matted surface. Water in thoroughly. Repeat annually for 2–3 years to build a meaningful clay content in the root zone. Once established, the clay is permanent and continues working without further application.
Fibre-based peat-free media have a very low CEC and hold nutrients poorly. Adding montmorillonite at 3–5 ml/L raises the effective CEC of the medium several fold, turning an inert sponge into a nutrient-retaining growing medium. Mix thoroughly before planting. Combine with sea shell meal or gypsum for calcium, and volcanic rock dust for trace elements. These media need all three to function as a complete growing medium.
Every time you water a pot of sandy compost, some of the nutrients you applied wash out of the bottom. Montmorillonite intercepts them and holds them in the root zone until the plant is ready. Each feed lasts longer, less is wasted, and you feed less often. Over time it can pay for itself in fertiliser you no longer need to buy.
Montmorillonite builds CEC. It does not supply trace elements or NPK. Pair it with Volcanic Rock Dust for trace minerals and Humic Acid Flakes for clay-humus complex formation; the three together are the mineral foundation of a living soil. If you would rather buy one bag, the Mineral Mix already includes clay minerals alongside gypsum, sea shell meal and basalt. Add a balanced feed such as All Purpose 4-4-4 or Bloom 2-8-4 for NPK, and Grow-Kashi for the biology that colonises the clay surfaces.
Keep the bag sealed, cool and dry. It draws moisture from the air and will clump if left open; clumps break up and work as normal. Indefinite shelf life. Keep out of reach of children and pets.
Mainly to give sandy soils and peat-free composts somewhere to hold nutrients and water. It's a swelling clay mineral with a cation exchange capacity of roughly 80–150 meq per 100 g, so its layers hold calcium, magnesium, potassium and ammonium that would otherwise wash through. Mix 2.5–5 ml per litre into potting compost and hanging-basket mixes, or rake it into hungry beds. It also helps keep compost heaps from smelling of ammonia. It doesn't decompose, so what you add this spring is still working years from now.
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Diastatic malted barley to feed soil enzymes and microbes.
from £10.99