How much does a cubic meter of soil weigh, and how many catties does a cubic meter of soil equal

How important is a cubic of soil 5261 to see what soil, because the density is different, generally cohesive soil =; Sand =; Humus = , which is the natural density. 4102 mass is equal to the product of volume and 1653 density (m = v), take one cubic clay as an example:

The general density of soil is.

g cm31 cubic meters is tons.

The specific gravity of saturated clay is about.

So the weight of 1 cubic meter of saturated clay is about tons.

Extended Materials. Cohesive soil refers to the version of the soil with more clay particles and less permeability. It has good water stability, high strength and large capillary action after compaction. Its particles are fine, the pores are small and weighty, the water permeability is weak, it has the characteristics of expansion and contraction, and the mechanical properties change with the water content.

General Cohesive Soil =

Sand =; Humus = , which is the natural density.

Mass is equal to the product of volume and density (m= v).

According to this formula, three types of soil weights can be calculated.

How much does a cubic meter of concrete weigh? The answer is terrifying to say it.

After compaction, ordinary loess exceeds tons per cubic meter (see density value). The density of dry soil (not compacted, generally used for greening) should be less than tons. The moisture content of the soil is the main factor to be considered, when the moisture content of ordinary soil is 5-7%, one side of the soil weighs tons.

The density of soil depends on the density of soil particles, the size of the pore volume and the amount of water in the pores, which comprehensively reflects the material composition and structural characteristics of the soil. Sand is generally tons per cubic meter ; clay is tonnes per cubic meter; peat bog soil is tonnes per cubic meter; So one square of soil is equal to 1400 kilograms.

Effect of dry density on subgrade performance.

1) The dry density has a significant effect on the soil-water characteristic curve, the larger the dry density, the smaller the saturated moisture content, the larger the air inlet value, and the stronger the water-holding capacity of the soil. The saturated moisture content decreases linearly with the increase of dry density, the residual moisture content increases linearly with the increase of dry density, the reciprocal correlation between parameter a and the inlet value, and the linear increase of parameter n with the increase of dry density.

2) The part of water discharged by the soil under the action of suction in the rapid dewatering stage is the free water in the soil, and the water discharged in the residual section is the combined water in the soil. The residual mass moisture content of the soil at different dry densities is constant.

3) The resilience modulus decreases with the increase of moisture content and increases with the increase of dry density, and the influence of moisture content on the resilience modulus is more significant than that of dry density.

The quality of the soil is related to the water content and compaction, and there is a difference between dense and loose, such as: digging earth, before digging is solid soil, after digging into virtual soil. Therefore: the earthwork mass is generally 1500-1800kg m.

After the ordinary loess is tamped, it is about more than tons per cubic meter (see the density value). The density of dry soil (untamped, generally greening soil) should be less than ton. General Cohesive Soil =Sand =; Humus = , this is the natural density, you can calculate it.

In addition, the moisture content of the soil is the main factor to be considered, when the moisture content of ordinary soil is 5-7%, one side of the soil weighs tons. Pebbles, crushed stones, gravel, sand and pebbles (dry and wet), fine sand (dry), coarse sand (dry), coarse and fine sand (wet), ordinary bricks, gypsum powder.

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1. After compaction, the ordinary loess exceeds tons per cubic meter (see the density value). The density of dry soil (not compacted, generally used for greening) should be less than tons.

2. Generally speaking, cohesive soil p= , sandy soil p = and humus soil p = are natural densities.

3. Natural compacted dry soil, the proportion of three types of soil is about 1 cubic meter and 2 tons, and the proportion of four types of soil is slightly larger.

The weight of the soil is also very related to the composition of chemical minerals, we mainly have to combine the density of the soil to calculate, if you want to measure the density of the soil, you also need to measure it in a formal way, you need to measure it many times when you measure, and then take the average value.

In general, the density of the graph is in the to.

The density of the soil is different, and the weight is different. When the density of the soil is g cm3, the weight of 1 cubic meter of soil is about tons, and the weight of 1 cubic meter of saturated clay is about tons. To claim the weight of the soil, it is calculated according to the product of the soil density, mass equal to volume and density (m = p v).

Cohesive soil refers to the soil with more clay particles and less permeability. It has good water stability, high strength and capillary action after compaction.

Big. Its particles are fine, the pores are small and many, the water permeability is weak, it has the characteristics of expansion and contraction, and the mechanical properties follow the water content.

size and variety.

Earthwork 4-5 yuan per square; The stone square is about 10 yuan.

tons or so. The density of the soil is different, and the weight is different. When the density of the soil is g cm3, the weight of 1 cubic meter of soil is about tons, and the weight of 1 cubic meter of saturated clay is about tons.

If you want to claim the weight of the soil, you should calculate it according to the product of the soil density, mass equal to volume and density (m = p v).

Cohesive soil refers to the soil with more clay particles and less permeability. It has good water stability after compaction, higher strength than collision line, and large capillary effect. Its particles are fine, the pores are small and many, the water permeability is weak, it has the characteristics of expansion and contraction, and the mechanical properties change with the water content.

How much does a cubic of soil weigh:

1. After compaction, the ordinary loess exceeds tons per cubic meter (see the density value). The density of dry soil (not compacted, generally used for greening) should be less than tons.

2. Generally speaking, cohesive soil p= , sandy soil p = and humus soil p = are natural densities.

3. Natural compacted dry soil, the proportion of less than three types is about 1 cubic meter and 2 tons, and the four types of soil are slightly larger than the mold trap case.

The density of soil is generally calculated in grams of cubic centimeters. 1 meter on the denominator is 100 centimeters, then 1 cubic meter is 1,000,000 cubic centimeters. The numerator and denominator of the density of the soil are multiplied by 1,000,000 to obtain 2,650,000 grams of cubic meters.

2,650,000 grams on the molecule is 2,650 kilograms, and another ton is 1,000 kilograms, so, 2,650 kilograms is a ton. So, the density of the soil is grams of cubic centimeters, and one side is tons. The type of soil is different, the density is different, after knowing the density, when the unit is gram cubic centimeter, its value is directly how many tons per square.

The density of the soil is related to the chemical and mineral composition of the soil.

General cohesive soil density:

Sand density: =;

Humus density: =.

According to the formula: mass is equal to the product of volume and density (m= v) For example: the density of general cohesive soil is taken, then the weight of one cubic soil x = tons.

Therefore, one side of the general cohesive soil is about a ton.

One cubic of earth is equal to a ton. The cubic is a unit of volume, the ton is a unit of mass, the units of the two are different, and they need to be calculated by density, taking the density of soil as an example per cubic centimeter, the volume is 1 cubic meter, and the formula for calculating the mass is: mass = density multiplied by volume.

According to the formula, 1 cubic meter is equal to 1,000,000 cubic centimeters; 1000000 cubic centimeters per cubic centimeter = 2800000g = tons, so one cubic of earth is equal to tons.

It is about equal to tons to tons, mainly because the density of the soil is also different, and there are some differences in the calculated weight.

One cubic of earth is equal to a ton. Because the density of soil is about one cubic meter.

The density of the soil is different, and the mass of the same volume will also be different, generally cohesive soil = ; Sand =; Humus = , which is the natural density.

It can be calculated by the fact that mass is equal to the product of volume and density (m= v).