The document discusses soil phase relationships and defines key terms. It describes how soil is composed of grains, water, and air which occupy volumes. The volume of voids is critical and affects other properties. Terms defined include void ratio, porosity, saturation, bulk density, saturated density, dry density, and relative density. Examples are provided to demonstrate calculating various phase properties from given data.
2. Soil Compositionمكونات التربة
Soil Grains (1حبيبات التربة
Voids: Water + Air (3 & (2
(الفراغات ) عبارة عن ماء وهواء
Soil Grain or
particle
Voids
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3. Void Ratio نسبة الفراغات
Vv
e=
Vs
Void, Vv
high e = Loose
سائب
Solid, Vs
low e = Dense
كثيف
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4. Saturation التشبع بالمياه
Vw
Sr = . 100
Vv
Air, Va
Voids, Vv = Vw + Va
Water, Vw fully saturated
Sr = 100 %
ا
ًمشبع تمام
Vv = Vw + Va Dry جافSr = 0 %
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5. Three Phases of Mineral Soils
Mineral soils are composed of:
Soil grains حبيبات التربة
Water مياه
Air هواء
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6. Weight Volume Relationships
Weight and volume of
soil sample depends on:
Specific gravity of soil
grains (solids) • Air
The size and space • Water
between soil grains
(voids and pores)
Volume of void space • Solids
filled with water
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7. PHASE DIAGRAM
To compute the masses (or weights) and
volumes of the three different phases.
Notation Va air Wa=0
W = weight الوزن
V = volume الحجم Vv
s = soil grains Vw water Ww
w = water Vt Wt
a = air
v = voids
Vs soil Ws
t = total
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Idealized Prism
7
8. Definitions
Water content (wc) ( (محتوى المياهis a measure
of the water or Moisture present in the soil.
Ww
wc = X 100% Vv
Va air Wa=0
Ws Vw water Ww
Vt Wt
Expressed as percentage.
Vs soil Ws
Range = 0 – 100+%.
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Phase Diagram
8
9. Definitions
Void ratio (e) ( (نسبة الفراغاتis a measure
of the volume of voids.
Va air Wa=0
VV Vv
e= Vw water Ww
VS Vt Wt
Vs soil Ws
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Phase Diagram
9
10. Definitions
Porosity (n) ( (المساميةis also a measure of the
volume of voids, expressed as a percentage.
Va Wa=0
Vv air
n= X 100%
Vv
Vw water Ww
Vt Vt Wt
Vs soil
Theoretical range: Ws
0 – 100%
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Phase Diagram
10
11. Definitions
Degree of saturation (Sr) ( (درجة التشبعis the
percentage of the void volume filled by water.
Va air Wa=0
VW
Sr = X 100% Vv
VV Vw water Ww
Vt Wt
Range: 0 – 100%
Vs soil Ws
Dry
Saturated
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Phase Diagram
11
12. Definitions
Bulk density (γ b) ( (الكثافة الكليةis the density of
the soil in the current state.
Va air Wa=0
Wt Vv
γb = Vw water Ww
Vt Vt Wt
Units: t/m3, g/cm3, kN/m3 Vs soil Ws
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Phase Diagram
12
13. Definitions
Saturated density (γ sat) ( (الكثافة المشبعةis the
density of the soil when the voids are filled
with water.
الكثافة المشبعة: هى كثافة التربة عندما تكون الفراغات مملوءة بالماء
Submerged density (γsub) ( (الكثافة المغمورةis the
effective density of the soil when it is submerged.
الكثافة المغمورة: هى كثافة التربة الفعالة عندما تكون مغمورة فى الماء
γsub= γsat - γw
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14. Definitions
Dry density (γ d) ( (الكثافة الجافةis the density of the soil
in dry state الكثافة الجافة: هى كثافة التربة فى الحالة الجافة
Va Wa=0
Ws air
γd = Vv
Vw water Ww
Vt Vt Wt
Units: t/m3, kg/m3, kN/m3
Vs soil Ws
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Phase Diagram
14
15. Phase Relations
Consider a unit volume of the soil solids,
where Vs = 1.
volumes masses
The other volumes can
be obtained from the
air
previous definitions. e
The weights can be Sre water Sreγw
obtained from:
Weight = Density x Volume
Ws γs Vs =1 soil Gsγw
γs = , Gs =
Vs
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γw Soil Phase Relationships
Phase Diagram
15
16. Phase Relations
Consider a unit volume of the soil solids,
where Vs = 1.
volumes masses
Vw Vw Vv
= x = Sr e air
Vs Vv Vs e
Ws Sre water Sreγw
= γ s = Gs γ w
Vs
Vs =1 soil
Vv Gsγw
e=
Vs
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Phase Diagram
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17. Phase Relationsالعلقات الظاهرية للتربة
From the previous definitions,
Vv e
n= =
Vt 1 + e e
air
Sr e water Sreγw
Ww S r e
wc = =
Ws Gs 1 soil Gsγw
Phase Diagram
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18. Phase Relations
Wt Gs + S r e
γb = = γw
Vt 1+ e
Wt Gs + e e
air
γ sat = = γw
Vt 1+ e Sre water Sreγw
Ws Gs
γd = = γw 1 soil Gsγw
Vt 1 + e
Phase Diagram
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19. Relative Density الكثافة النسبية
It is a measure of the soil state of
compactness, and expressed as:
e max - e
Dr =
e max - e min
هى الكثافة النسبية وهى حالة الدمك وتستخدم غالبً فى التربة
ا
الرملية
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20. EXAMPLE 1
A sample of saturated clay has a water content Wc = 47.0%
and specific gravity Gs = 2.7. Calculate the voids ratio e, the
porosity n, and the saturated unit weight γsat.
Wc x G s Gs + e
e= γ sat = x γw
Sr 1+ e
0.47 x 2.7 2.7 + 1.27 3.97
e= = 1.27 = x1=
1 1 + 1.27 2.27
e
n=
1+ e
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21. EXAMPLE 1
Solution Using Prism:
Vv 0.47
e= = = 0.47x2.7 = 1.27
Vs 1
2.7
Vv 0.47
n= = = 0.56
Vt 0.47 + 1
2.7 Vv = Vw Ww =
W water
γ sat = = = 0.47 0.47 gm
V
0.47 + 1
= 1.75 gm/cm3 Vs = soil
1 ws= 1.0
0.47 +
2.7 1/2.7
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22. EXAMPLE 2
The weight of a wet specimen of clay is 34.62 gm. The dry
weight = 20.63 gm. Before drying, the specimen was
immersed in mercury and its volume was found to be 24.26
cm3, if Gs = 2.7, calculate the water content Wc, the voids
ratio e, and the degree of saturation Sr.
Solution:
Ww = 34.62 - 20.36 = 14.26 gm
Ww 14.26
Wc = %= x 100 = 70.40%
Ws 20.36
Water content, Wc = 70.40%
where
20.36
Vs = = 7.54 cm3
2.7 x 1.0
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23. Vv = V - Vs
Vv = 24.26 - 7.54 = 16.72 cm3
Vv 16.72
e= = = 2.22
Vs 7.54
Voids ratio, e = 2.22
Vw
Sr = %
Vv
14.26
Sr = 1 x 100 = 85.29 %
16.72
Degree of Saturation, Sr = 85.29%.
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