
The
Sky Garden Intensive Green Roof system is designed to use a soil-base that will compliment the plants selected
for the Green Roof. This means that several
different soil mixes may be appropriate for a Sky Garden depending on the plants
selted. However, G-SKY has developed a lightweight soil mix that
will support 95% of all plants on the roof environment for decades.
Roof
Soil™ is a lightweight specially-mixed soil with a saturated weight
of only 44~50 lbs/ft³ (specific gravity = 0.7~0.8)! It is almost half the weight of traditional landscape soil or naturally-occurring
soil.
The G-SKY Extensive Green Roof System is designed to use
Roof Soil™ 2,
a lightweight specially-mixed soil.

Roof Soil™ products are comprised of completely natural 100% organic materials. They consist
of naturally-derived pumice, USGA well-graded sand and aged composted bark mulch.
Because of their natural states, none of these materials require the use of fossil-fuels
in their production. Because of their lightweights,
use of fuels in derivation, transport and mixing is very low, resulting in the
CO
2 production volume to install Roof Soil™ products on roofs or the ground much less
than to install traditional landscaping soils or naturally occuring soils.

Roof Soil™ products are approximately one half the weight of regular landscaping
or naturally-occurring soils which significantly reduces their burden on a building.
EPA Clean Water Act: 30mm and 100mm rain storms were simulated
onto beds of Roof Soil™ products. The quality of the drained water was well
above the water quality standards dictated by the EPA's Clean Water Act for all
contaminants in surface waters.
Skin Abrasion Test: Due to the increase in Green Roof and balcony
popularity, the number of people coming into contact with soil products is increasing.
Several of the soils used for Green Roofs contain substances such as artificial
fertilizers or mycorrihizae inoculants to produce a healthy growth environment for
plants, but are toxic or harmful to humans. Roof Soil™ products were tested
for these substances and its toxicity towards humans in several skin stimulus tests.
In dry and wet condition soil to skin tests, Roof Soil™ products produced
no sign of erythema (redness of the skin caused by dilation and congestion of the
capillaries), scabbing or anasarca (accumulation of fluids in the skin tissue).
Roof Soil™ products are considered safe for general handling without the need
for further protection.
Toxicity Report: Roof Soil™ products were tested on mice
to identify toxicity if ingested. In all cases, no abnormal weight, movement
ability or breathing ability changes were noted. All internal organs were
in perfect health and there was no sign of toxicity in the internal organs of the
mice. Roof Soil™ products are not harmful to humans if ingested.

Roof Soil™ products have a good water holding capacity without
compromising permeability. In addition, it is a very structurally stable soil.
If properly blown and compacted into place, it can be safely installed on
30~35° slopes with little to no additional soil support structures installed.

Installing soil onto a building requires careful planning and established installation/safety
protocols. During installation, soil can easily be scattered by the wind causing
damage or annoyances to neighboring buildings and the streets below. Roof
Soil™ products are delivered slightly damp in order to prevent scattering in the
wind. Furthermore, Roof Soil™ is unlike natural soil in that it does not become
muddy in the rain, therefore making installation in the rain possible.

Roof Soil™ used on Sky Garden Green Roofs is designed to suit the growth conditions
of 95% of all plants
while still being lightweight. If particularily odd plants
are used, a specially designed soil mix may need to be employed.
The soil used on a G-SKY Green Roof, which employs a thin soil-base, must be designed
to provide drought tolerant/shallow rooted plants a healthy growth environment, has an adequate available moisture
content for the plants (when used in conjunction with G-SKY Drain) and drains quickly
enough to prevent root rot.
Presented below is a summary of the differences between
Roof Soil™,
Roof Soil™ 2 and naturally-occurring soils.
Roof Soil™ Products Compositions:
1)
Roof Soil™ : Pumice, USGA Well-Graded Sand, Aged Bark Compost
2) Roof
Soil™ 2 : Pumice, Aged Bark Compost
|
Measurement |
Unit |
Results |
|
Roof Soil™ |
Roof Soil™ 2 |
Naturally- occuring Soil |
Landscape
Soil |
|
Size Distribution |
|
25mm sieve
80% passed |
19mm sieve
80% passed |
|
|
Fully-saturated Weight
(pF 1.8) |
Specific
Gravity
(lbs/ft³) |
0.79±0.05
(50) |
0.7±0.05
(44) |
1.6~1.8
(100~112) |
1.6~1.8
(100~112) |
Thermal Conductivity
Coefficient |
W/m·K
(btu/ft·h·°F) |
0.42
(0.24) |
0.42
(0.24) |
- |
- |
Three
Phase
Distribution
Ratio |
Voids |
% |
45±5 |
45±5 |
See the diagram below |
Varies greatly depending on producer |
|
Liquids |
% |
35±5 |
25±5 |
|
Solids |
% |
20±5 |
30±5 |
Available Water
Capacity
(pF 1.8~3.0) |
Liters/m³
(Gallons/yrd³) |
150±30
(30±6) |
100±20
(19±4) |
Chernozem:
80~140
(16~28)
Sandy Loam:
100~150
(19~30) |
80~150
(16~30) |
|
Permeability Coefficient |
cm/s |
1 x 10-2
|
1 x 10-4 |
1 x 10-2 ~
1 x 10-5 |
1 x 10-2 ~
1 x 10-5 |
|
pH (H2O) |
- |
6.0~7.0 |
6.0~7.0 |
5.0~6.0 |
5.5~7.0 |
Cation Exchange Capacity
(CEC) |
milliequivalents
per 100 grams (me) |
20.1 |
43.7 |
- |
Varies greatly depending on producer |
|
Referenced standards:
ASTM C127/C128-Test Method for Density, Relative Density (Specific Gravity), and
Absorption of Fine/Coarse Aggregate.
ASTM E11-Specification for Wire Cloth and Sieves for Testing Purposes T19/T19M
Method of Test for Unit Weight and Voids in Aggregate.
ASTM D2216 Test Method for Laboratory Determination of Water (Moisture)
Content of Soil and Rock by Mass.
ASTM D854 Test Method for Specific Gravity of Soils. ASTM
D5334-05 Standard Test Method for Determination of Thermal
Conductivity of Soil.
|
Chart
Description
|
1) What is the Fully-saturated
Weight (pF 1.8) value? |
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|
This value, pF 1.8, represents the weight of the soil when the soil is has reached
the water saturation point where it can no longer hold water within its structure
withstanding the force of gravity. A pF curve defines soils moisture characteristics:
{a} amount of water available for plants and {b} available water capacity of the
soil. A value of ‘pF 1.8’ is a soils “field capacity”, the maximum amount of water
a soil can hold withstanding gravity. ‘pF 4.2’ is the “permanent wilting point”, which is
when the soil is so dry that plants roots can no longer generate sufficient suction
to obtain further water from the soil, and therefore begin to wilt.
See the chart in question 3 for more details. |
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2) What is the Three-Phase Distribution
Ratio? |
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Soil
is a three-phase, porous media, composed of solids, liquids, and voids (empty spaces
between the solids). This ratio describes the structure of the soil quantitatively.
It exposes the soils compaction ratio, provides a method by which to calculate the
water holding capacity, and water/air permeability. The typical amount of
total porosity (ratio of void volume to total volume) in a mineral soil ranges from
about 40% to 60%. This means approximately 40 to 60% of the volume of a mineral
soil is actually empty space between the solid particles (voids). These voids
are filled with air and/or water. The air of soil is quite different that that in
the atmosphere. In the atmosphere, oxygen comprises about 21% and carbon dioxide
comprises about 0.36%. However, in the soil, the oxygen levels are generally less
than atmospheric levels and the carbon dioxide levels are generally greater than
atmospheric levels (with the major of the air consisting of nitrogen gas, ~78%).
Furthermore, the air in soil has a relative humidity of almost 100% all of the time
(relative humidity is the amount of water vapor actually in the air relative to
the amount air can hold at a given temperature).
Below is a description of each phases:
(1) Solid Phase: If the solid phase ratio is too high then space for roots
to grow become limited and growth is stunted.
(2) Void: If the void phase ratio is high the roots cannot absorb oxygen
due to excess moisture and root rot occurs.
(3) Liquid: If the liquid phase ratio is high, the soil will easily
dry out, and the plants will wither.
Roof Soil products are closest in its physical characteristics to Volcanic Ash Soil,
the most fertile soil in the world. Sand-based soils have little moisture
and a great deal of air making them unsuitable. Alluvial and Diluvial soils
consist of far too much solid material to support healthy root growth making them
also unsuitable.
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3) What is the Available Moisture
Capacity of soil? |
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What does it mean to measure the soils fully-saturated weight at pF 1.8? The
moisture state of soil between being wet and dry is described by this chart:

It is important to keep the soils moisture above its wilting point, pF 1.8~3.0,
in order to not place stress on the plants. Capillary action of water stops
around pF 2.7~3.0 providing little benefits to the roots of the plants unless they
are in direct contact with the water in its stopped state. Water is actively
moving by capillary action in soil around pF 1.8~3.0, and therefore when an adequate
volume of water exists in the soil to allow for movement by capillary action, it
is referred to as the soil's "effective water content".
It is important to note that the moisture characteristics of soil are effected by
several factors:
- Rock Fragments: reduce capacity in direct proportion to their size (i.e. gravel),
unless the rocks are porous (i.e. pumice or lava rock)
- Organic Matter: increases water capacity. The type dictates how much will
be increased by the quantity added, however, approximately 1% of organic matter
increases the available water capacity by 1.5%
- Bulk Density: dictates pore space available to hold water. High bulk
densities tend to lower available water capacity.
- Osmotic Pressure: equal to 0.3~0.4 times the electrical conductivity in mmhos/cm.
Reduces the available water capacity when the electrical conductivity is 8 mmhos/cm
or more.
- Texture: different types of soil textures effect available water capacity.
Sandy soils have a low capacity, but as silts and clays are added to the soil the
capacity increases significantly.
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4) What is the Permeability
Coefficient of soil? |
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The permeability coefficient of soil represents the speed at which water can travel
through the soil, expressed in metric as centimeters per second, this value is never
expressed in imperial inch/sec units. Permeability rates
allows us to calculate irrigation system requirements and drainage. The relation between
the permeability coefficient and a soil's water permeability is as follows:
|
Permeability Coefficient (cm/s) |
Soil's Water Permeability |
Comparable To: |
|
10-2 |
Excellent |
Clean Sand |
|
10-3 |
Good |
Clean Sand |
|
10-4 |
Good |
Mixed Sand |
|
10-5 |
Low |
Dirty Sand |
|
10-6 |
Almost Impervious |
Heavy Silts |
|
10-7 |
Impervious |
Hard Clay |
Natural soil and traditional landscaping soil permeability changes drastically from soil to soil, however, Roof
Soil™ products have consistent permeability coefficients of 10-2 and
10-4.
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5) pH (H2O)? |
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pH of soil is measured by passing a distilled water through soil to expose the soils
pH(H2O). It is also often measured using a potassium chloride solution and
in these cases is expressed as pH(KCl).
The effect of soil pH is great on the solubility of minerals or nutrients. Fourteen
of the seventeen essential plant nutrients are obtained from the soil. Before a
nutrient can be used by plants it must be dissolved in the soil+water solution. Most minerals
and nutrients are more soluble or available in slightly acid (5.0~7.0)
soils than in neutral (7.0) or slightly
alkaline (>7.0) soils.
Phosphorus is never readily soluble in the soil but is most available in soil with
a pH range centered around 6.5. Extremely and strongly acid soils (pH 4.0~5.0) can
have high concentrations of soluble aluminum, iron and manganese which may be toxic
to the growth of some plants. A pH range of approximately 6.0~7.0 promotes the most
readily availability of plant nutrients. Roof Soil™ products have a pH of 6.0~7.0. |
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6) What is the Cation
Exchange Capacity? |
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Represents a soils ability to hold nutrients. The CEC of a soil is not easily adjusted
and therefore must be designed into the soil mix. If this value is high, the ability
for plants to absorb nutrients increases. If it is low, adding fertilizer may be
a wasted exercise and plant growth, flowering and seeding will be very low.
A good value for Green Roof soil is 6me+.
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