Bulk density and porosity relationship

Porosity - Wikipedia

bulk density and porosity relationship

The bulk density values ranged from to and the porosity from to Keywords: bulk density, correlation coefficient, micro-structures, porosity, . Table 1: The relationship between compaction, apparent density and porosity. Degree of. Apparent. Total. Macro. Micro. Compaction. Density. Porosity. Porosity . Download scientific diagram | Relationship between Bulk density and porosity from publication: Effects of Mulching on Soil Hydro-Physical Properties in Kibaale .

This calculates to a porosity between 0. Typical bulk density of clay soil is between 1. This seems counterintuitive because clay soils are termed heavy, implying lower porosity.

bulk density and porosity relationship

Heavy apparently refers to a gravitational moisture content effect in combination with terminology that harkens back to the relative force required to pull a tillage implement through the clayey soil at field moisture content as compared to sand. Porosity of subsurface soil is lower than in surface soil due to compaction by gravity. Porosity in finer material below the aggregating influence of pedogenesis can be expected to approximate this value.

bulk density and porosity relationship

Soil porosity is complex. Traditional models regard porosity as continuous.

WM Earthcare » Everyday Soil Science #4: Bulk Density & Porosity

This fails to account for anomalous features and produces only approximate results. Furthermore, it cannot help model the influence of environmental factors which affect pore geometry. A number of more complex models have been proposed, including fractalsbubble theory, cracking theory, Boolean grain process, packed sphere, and numerous other models. The characterisation of pore space in soil is an associated concept. Types of geologic porosities[ edit ] Primary porosity The main or original porosity system in a rock or unconfined alluvial deposit.

bulk density and porosity relationship

Secondary porosity A subsequent or separate porosity system in a rock, often enhancing overall porosity of a rock. This can be a result of chemical leaching of minerals or the generation of a fracture system.

This can replace the primary porosity or coexist with it see dual porosity below. Fracture porosity This is porosity associated with a fracture system or faulting. This can create secondary porosity in rocks that otherwise would not be reservoirs for hydrocarbons due to their primary porosity being destroyed for example due to depth of burial or of a rock type not normally considered a reservoir for example igneous intrusions or metasediments. Vuggy porosity This is secondary porosity generated by dissolution of large features such as macrofossils in carbonate rocks leaving large holes, vugsor even caves.

Effective porosity also called open porosity Refers to the fraction of the total volume in which fluid flow is effectively taking place and includes catenary and dead-end as these pores cannot be flushed, but they can cause fluid movement by release of pressure like gas expansion [3] pores and excludes closed pores or non-connected cavities.

This is very important for groundwater and petroleum flow, as well as for solute transport. Ineffective porosity also called closed porosity Refers to the fraction of the total volume in which fluids or gases are present but in which fluid flow can not effectively take place and includes the closed pores.

bulk density and porosity relationship

Understanding the morphology of the porosity is thus very important for groundwater and petroleum flow. Dual porosity Refers to the conceptual idea that there are two overlapping reservoirs which interact. In fractured rock aquifers, the rock mass and fractures are often simulated as being two overlapping but distinct bodies. Clays also increase water storage by providing an abundance of micropores. Thus, texture and structure, plus the level of induced compaction, are the main properties governing amount and type of pore space in the soil.

Organic matter affects porosity through its enhancement of soil aggregation. Porosity can be calculated if bulk density and particle density are known. Bulk density is soil mass divided by unit volume. In its natural state, a soil's volume includes solids and pores, therefore, a sample must be taken without compaction or crumbling to correctly determine bulk density.

It increases with depth and tends to be high in sands and compacted pan horizons, and tends to be low in soils with abundant organic matter. Tillage operations looen soils and temporarily lower bulk density, while compaction processes raise bulk density. High bulk densities correspond to low porosity. Natural soil-forming processes that increase aggregation reduce bulk density, but excessive tillage and raindrop impact on bare soil destory aggregation and increase bulk density.

Particle density is the volumetric mass of the solid soil. It differs from bulk density because the volume used does not include pore spaces. For most soils, this value is very near 2. Particle density varies little between minerals and has little practical significance except in the calculation of pore space.

Porosity is that portion of the soil volume occupied by pore spaces. This property does not have to be measured directly since it can be calculated using values determined for bulk density and particle density. A cm3 cylindrical container was used to collect an undisturbed soil sample.

The container and soil weighed g when dried. When empty the container weighed 75 g. What is the bulk density and porosity of the soil?

Bulk Density