Saponite. Characteristics, distribution, application
Saponite is an amorphous mineral similar to montmorillonite. Its structure is represented by scaly, earthy, clay-like dense masses, as well as fibrous aggregates, spherulites and occasionally small stalactites. When wet, it is soft and greasy to the touch, and when dry, it forms a dense porous mass. The mineral is characterised by perfect cleavage along the (001) plane.
Saponite is included in the list of minerals of national importance approved by the Resolution of the Cabinet of Ministers of Ukraine dated December 12, 1994, No. 827, as a raw material for agrochemicals and mineral pigments.
Physical and chemical properties
Saponites (magnesium smectites) are a group of trioctahedral finely dispersed layered silicates and aluminosilicates of the 2:1 structural type. They belong to the montmorillonite group, where Al³⁺ is almost completely replaced by magnesium in the octahedral lattice of the mineral, and Si⁴⁺ in the tetrahedral lattice is partially replaced by Al³⁺. Saponites are characterised by a swelling structure and high sorption properties.
Chemical formula Mg3[(OH)2|Al0.33Si3.67O10]•nH2O.
Approximate composition of saponite: SiO₂ — 39.6–54.7%, Al₂O₃ — 3.9–10.2%, MgO — 15.8–33.3%, Fe₂O₃ — 0.2–12.0%, FeO — 0–7.8%, CaO — 0–2.9% , Na2O — 0–0.7%, K2O — 0–0.3%, TiO2 — 0–0.4%, MnO — 0–0.3 H2O + (structural water OH) — 4.2–12.0, H2O-(hydration water) — 7.2–17.4.
The colour of saponite clays varies from yellowish to brown or greyish-green, and the fracture is uneven.
Laboratory studies have revealed the following physical properties:
- actual specific gravity: 2.65–2.97 g/cm3,
- average density — 1876–2160 kg/m3,
- plasticity — 28.4
- hardness on the Mohs scale — 1.5–2.5,
- porosity — 23.13–36.82%,
- water absorption — 11.79–25.01%,
- moisture content — 23.33%,
- refractoriness — 1280–1300°C,
- looseness coefficient — 1.67.
Saponite and saponite-bearing rocks consist mainly of layered aluminosilicates. The main rock-forming mineral is trioctahedral smectite-saponite. Small amounts of dioctahedral smectite (up to 7–10%), analcime (up to 35% in the lower horizon, 3–8% in the upper horizon), as well as calcite, hematite, quartz, anatase and chlorite.
Distribution of saponite
Industrial deposits of saponite raw materials were first discovered in Ukraine in the 1970s on the western slope of the Ukrainian Shield, where saponite clays form the bentonite province. Here, they are confined to the weathered crust of basalt tuffs of the Volyn series of the Vendian period.
In the Khmelnytskyi region, four deposits of saponite clays have been explored: Tashkivske‑I, Tashkivske-II, Radoshivske and Varvarivske, with total reserves estimated at 10–20 million tonnes. Saponite is already being mined at one of the deposits in a small quarry, and the product is processed in the city of Slavuta.
The saponite and saponite-bearing rocks of the Varvarivske deposit are mainly represented by a highly dispersed clay mineral. In the upper horizon (depth 20–40.9 m), the saponite rock is brown or dark brown in colour, loose when dry, sometimes friable, with thin, compacted, horizontally layered interlayers of greenish and light grey tones. In the lower horizon (depth 40–70 m), the rocks are dense, monolithic, dark brown in colour and have a conchoidal fracture.
The quality assessment of saponite from the Varvarivskyi deposit is based on the requirements of industry technical conditions approved by the head of the State Department of Veterinary Medicine of the Ministry of Agrarian Policy of Ukraine, registered at the Khmelnytskyi State Centre for Standards, Metrology and Certification under No. 102/000952 — TU U 24.4–13973968-003‑2003 ‘Saponite flour ’Sapokorm”. According to the technical specifications, saponite flour is used in animal husbandry and poultry farming as a natural mineral prophylactic and therapeutic feed additive, a growth and health stimulant for animals and poultry, and as a sorbent.
According to the lithological section, the Varvarivske deposit is represented by the following layers:
- Cover layer — limestones, limestone sandstones (up to 0.6 m);
- Bentonite rocks (4.5–6 m);
- Siliceous rocks (up to 1–1.5 m);
- Saponite layer (up to 70–80 m).
By analogy with the Varvarivskyi deposit, the mineral resource of the Tashkivska‑1 site is represented by a stratiform deposit of argillaceous saponite clays of the Babynska Formation of the Vendian, confined to the weathering crust of basalt tuffs of the Berestovets Horizon of the Volyn Series of the Lower Cambrian, dense, with well-preserved structural features of tuffaceous rock fragments, brown, reddish-brown, greenish and grey in colour, thin-layered texture, with a thickness of 17.0 to 40.3 m. The overburden rocks include chalk deposits represented by flint nodules cemented with sandy-clayey material, chalcedonolites, Quaternary sands and a soil-plant layer with a total average thickness of 18.4 m.
Uses of saponite
Saponite, enriched with chemical elements such as aluminium, calcium, iron, hydrogen, magnesium, oxygen, titanium, manganese, sodium, potassium and phosphorus, has a wide range of applications in agriculture and industry. Due to its properties, it is used for mineral feeding of animals, as a preservative for green fodder, and as a feed improver. Saponite is also effective for the reclamation of land contaminated with radionuclides.
The magnesium variety of saponite clays, also known as bentonite clays, is widely used in more than 80 industries in developed countries. They are an important component of international export and import operations, which indicates their high economic value. Ukraine, for example, needs more than 4 million tonnes of saponite raw materials annually, of which 3 million tonnes are required for livestock farming alone.
Saponite clays can serve as natural fertilisers that help increase yields of corn, wheat, rye and other grain crops. In particular, the high magnesium content in saponite and its neutralising properties can significantly increase the yield of sod-podzolic soils, which occupy a significant part of the arable land in the Ukrainian Polissya region.
Saponite and glauconite can be used in feeding broiler chickens as additives or components of compound feed in an amount of 4–6% of the total feed mass. The use of these natural minerals has a positive effect on the digestive system of poultry, in particular, it contributes to an increase in feed nitrogen absorption by 1.0–1.3% and improves fibre digestibility. Due to their properties, saponite and glauconite slow down the passage of feed through the gastrointestinal tract, which reduces the moisture content of the feed in the intestine by 1.2–3.8%.
In addition, these minerals have a positive effect on the physiological state of broilers. They contribute to an increase in vitamin A content in the liver by 33.4 μg, increase the level of fatty acids in the diet by 0.12–4.06% and increase the concentration of haemoglobin in the blood. As noted by M.F. Kulik, the introduction of saponite and glauconite into the feed of farm poultry contributes to an increase in the survival rate of broiler chickens by 1.0–2.0%, their live weight by 0.9–7.4%, and also reduces feed costs per unit of growth by 1.2–7.4%.
Based on saponite raw materials, Ukrainian scientists have created a feed additive called ‘Fistashki’, which is produced by the experimental plant of the Vinnytsia Scientific and Production Association ‘Mindozyviva’. This product is widely used in animal husbandry to improve the diet of animals and birds.
In pharmacology, saponite is used as an adsorbent, viscosity-enhancing agent, suspending agent or emulsifier, and is useful as a structural component in semi-solid cosmetic and medical products. It is also used in the development of gastrointestinal X‑ray contrast agents and preparations intended for prolonged delivery to the gastrointestinal tract.
LET’S COMPLETE ROUTE FROM IDEA TO MINING BUSINESS TOGETHER
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