All About Marginal Soils
Part 1 of 3: How Soils Are Broken

Urban soils are typically inhospitable places for trees, other plants, and their oxygen breathing microorganisms. Construction equipment, grading, and even human foot traffic leave urban soils much more compacted than natural soils. Typically 40-55% of the volume in a healthy forest soil consists of pore space. This pore space consists of varying proportions of air and water depending on the weather. With compaction, soil particles are pushed together and fill up pore spaces, so pore space in urban soils often goes down to 20-30%.

Soil compaction is generally estimated by measuring bulk density, which is the mass of dry soil divided by its volume, expressed in grams per cubic centimeter (gms/cc).  Compacted soil has less pore space and therefore higher bulk density. Surface bulk density of most undisturbed soils ranges from 1.1 to 1.4 gms/cc, depending on the soil texture (clay, sand and silt fractions). The bulk density of urban soils often ranges from 1.5 to 2.0 gms/cc, just slightly less than the bulk density of concrete (2.2 gms/cc)!

The reduced porosity of compacted soils results in a lower water holding capacity and reduced infiltration rate, so compacted soils produce much more stormwater runoff than undisturbed soils. In many urban areas, pervious areas, like lawns, produce almost as much runoff as impervious surfaces because they are so compacted. The reduced water holding capacity of compacted soils also renders plants more prone to drought and results in more extreme summer soil temperatures.

Compaction also drives oxygen out of these soils to suffocatingly low levels and oxygen dependent soil microorganisms can no longer survive. Not surprisingly, urban soils also generally have a lower organic matter content and lower nutrient retention than natural soils.

Soil compaction also limits root and hence plant growth. Once soil bulk density exceeds 1.4-1.7 gms/cc (depending on soil texture), roots are no longer able to penetrate soil, and vegetation growth becomes limited.

Bulk densities typically remain about 0.3 to 0.4 gms/cc above predevelopment levels after development. Urban pervious areas with extensive foot or vehicular traffic after development continue to become more compacted after development, with surface bulk densities often ranging from 1.9 to 2.1 gms/cc.

In parts two and three of this series, we’ll discuss whether soil compaction can be reserved or prevented.

Part II: Can Broken Soil Be Fixed?
Part III: What This Means For Silva Cell Projects

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