Red volcanic lapillus in sand, volcanic lava 0/3 mm (pallet of 45 bags of 33 lt)

RED VOLCANIC LAPILLUS IN SAND, VOLCANIC LAVA 0/3 mm (pallet of 45 33 lt bags) .

Substantially it is an effusive magmatic mineral (vulcanite from the Pleistocene period) naturally calcined at high temperature, porous, insulating, light .

P omice and lapilli are the product of explosive volcanic eruptions formed following a violent expansion of gases dissolved in lavas of acidic chemical composition: the rapid cooling of the rock prevented its crystallization, trapping the gases inside and generating honeycomb minerals expanded in a more or less concentrated manner.

In fact, during the solidification phase, the vapors present in the magma, suddenly released, caused the swelling of the entire mass of the magma and it is during this rapid cooling phase that the differences in the physical structure of the various volcanic aggregates were determined: the volcanic lapilli it was formed from a magma with a lower silica content.

The lower viscosity and the slower cooling of the lava facilitated the escape of a certain quantity of the gases present in the magma.

Minerals were formed characterized by voids with an average diameter greater than those of pumice but of a decidedly lower number.

CHEMICAL-PHYSICAL CHARACTERISTICS

DENSITY: 950 - 1150 Kg/m3 (quarry humidity);

WATER RETENTION: from 8 to 13% by volume (available/useful water);

AVAILABLE WATER: from 6 to 9% by volume;

CSC: approximately 18 meq/100 g;

ACTIVE LIMESTONE: free;

pH: 7 - 8;

NON-TOXIC PRODUCT: (free from crystalline free silica) .

MEDIA CHEMICAL ANALYSIS

SiO ₂ : 56%;

Al ₂ O ₃ : 16.5%;

_2O : 4.9%;

Fe ₂ O ₃ : 6.5%;

CaO: 8.8%;

Na ₂ O: 2.2%;

TiO ₂ : 0.8%;

MgO: 3.1%.

IDEAL FOR

? Rooting cultural substrates;

? Draining substrates for sports fields (football, tennis, etc.);

? Stabilized draining for clay surfaces;

? Mulches;

? Preparation of potting mixes;

? Soilless crops;

? Thermal and acoustic insulation;

? Soil amendment;

? Mineral layer for bio-filtration.

FUNCTIONAL CHARACTERISTICS

Material particularly suitable for creating drainage, ideal for lawns, in sports facilities, for all construction techniques:

? Ex DIN standards in all variants;

? STRI standards;

? USGA drainage;

? Reinforced drainage;

? Vertical drainage.

N B: NEWS ON COLOR

Please note that the color of the material is variable. It depends on many factors including: the extraction point in the quarry and the humidity contained. In color it varies from light red-purple (when the product is totally dry) to intense red-brown (when the product is humid or wet). It is not possible, in any way, to choose between these colors which are found without distinction inside the product. The secondary photograph of this listing, where the product is held in the hand, demonstrates the variability of the shades. By observing advertisements with grain sizes different from this one, it is possible to appreciate the color variations which are mainly given by the degree of humidity of the material at the time the photograph was taken.

NB: SHIPPING INFORMATION

THE PALLET FOR SALE WEIGHS 1,800 KG, THEREFORE IT CANNOT BE UNLOADED BY THE COURIER IN CHARGE OF DELIVERY WITH THE HYDRAULIC TAIL TAILS OF THE TRUCKS (THE HYDRAULIC TAIL TAILS OF TRUCKS CAN UNLOAD UP TO A MAXIMUM OF 1,200 KG) SO IT WILL BE THE BUYER'S RESPONSIBILITY TO PROVIDE THIS UNLOADING THE PALLET USING YOUR OWN VEHICLES (FOR FORKLIFTS, MECHANICAL LOADERS EQUIPPED WITH FORKS OR TRACTORS EQUIPPED WITH FORKS ABLE TO LIFT THE WEIGHT IN QUESTION).

NB: AVAILABILITY OF THE MATERIAL

The material is subject to availability, it is usually collected from the quarry and shipped to the customer in order to always have a clean product in excellent condition. We therefore ask our customers to check availability and delivery times by contacting Geosism & Nature.