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Problem Soils

Cohesive (Clay) Soils

   Earlier, we made mention of clay soils, but at that time we made no effort to say much about it, so now lets cover some important aspects about this topic, and see what we can glean or derive from these interesting facts.

   Like granular soils; clayey soils (Cohesive) are also, from combinations of various soil particles that range in size and shape from fine-grained to very-fine-grained, some of these clay particles cannot even be seen under a low-powered microscope.Cohesive soils are held together by a binding force called cohesion.

    Under the classification system devised by the American Society for Testing and Materials (ASTM) describe this second group, Cohesive soils as follows;

   Cohesive: (Fine-grained soils 50% or more passes the 0.075 mm #200 sieve.)

   The cohesive group symbols Silts and Clays Liquid Limit 50% or less are:

  • "ML"; Inorganic silts, very fine sands, rock flour, silty or clayey fine sands
  • "CL"; Inorganic clays of low to medium plasticity, gravely/sandy/silty/lean clays
  • "OL"; Organic clays of medium to high plasticity

   The cohesive group symbols Silts and Clays Liquid Limit greater than 50%:

  • "MH";Inorganic silts, micaceous or diatomaceous fine sands or silts, elastic silts
  • "CH"; Inorganic clays or high plasticity, fat clays
  • "OH"; Organic clays of medium to high plasticity
  • Peat: Highly Organic Soils; "PT"; Peat, muck, and other highly organic soils

    I felt it necessary to go the extra mile, and also decided that we had to cover clay soil at some length to get some since of the need to understand why they are termed " Problem Soils or Expansive Soils",and why stress is placed so heavily concerning this topic. We have to better understand the natural tendencies of clay soil due to the fact that they directly affect stability. This stability, with respect to foundation support, is of utmost importance and what precautionary steps we should take to alleviate or counter the reactions that are associated with this soil type.

   Clayey soil, termed problem soils, are said to be not suitable forengineering needs. What's the reason for all the controversy? The reasons are, these soils are the main culprit to so much foundation trouble, seeing  that the stability of these clays is directly affected by natural occurrence (climate). They become plastic and elongate under stress, impervious, poor drainage, high susceptibility to frost action, and low bearing capacity.  And the major problem with clay soils, is a characteristic behavior that is common to clay soils and that is; these clays contain mineral constituents that as variations in natural ambientconditions (heat, rain, wind, and conditions that result from water leaks in the sub-soils) cause these minerals to swell with higher  moisture content and contract in areas of widely variant moisture, and this problem is compounded by an interaction of these climatic changes.

   This swelling is directly attributed to a mineral,montmorillonite orsmectite present in the soil and changes or swells with moisture content. Montmorillonite when taken from a dehydrated state to a saturated state has the capacity to free swell up to 20 fold. So a confined clay for example under a foundation or concrete pad; these clays could conceiveably exert pressures up to several tons per square foot, and that; my friend, is

the reason that foundation repairs exceed or equal to the cost of damages due to natural disasters.  The last I read was 2 billion.

                      Let me know what you think.  Have a good day!!

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Posted in Analysis, Soil, cohesive, soil profile.

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Soil Stability


What Kind of Dirt Is That??

I'm going a little off track, but not far. I wanted to talk some on sands because we haven't covered that yet and also, I'm not quite through with clays, so the USCS will  have to suffice for the moment and then back to expansive clays.  (I did give you a heads up)

  For an in-depth coverage, let us look again at the chart of the Unified Soil Classification System Symbols. Broken down into four groups, and rated excellent to poor; we have:

Group I  (Excellent)   

GW  

  • Well-graded-gravels, gravel-sand mixtures, little or no fines.
  •  Allowable bearing capacity in pounds per square foot with medium  compaction or stiffness: 8000.
  • Drainage Characteristics: Good.
  • Frost heave potential: Low.
  • Volume change potential: Low.

GP

  • Poorly-graded-gravels, or gravel-sand mixtures, little or no fines.
  • Allowable bearing capacity in pounds per square foot with medium compaction or stiffness: 8000.
  • Drainage Characteristics: Good.
  • Frost heave potential: Low.
  • Volume change potential: Low.

SW

  • Well-graded-sands, gravelly-sands, little or no fines.
  • Allowable bearing capacity in pounds per square foot with medium compaction or stiffness: 6000.
  • Drainage Characteristics: Good.
  • Frost heave potential: Low.
  • Volume change potential: Low.

SP

  • Poorly-graded-sands or gravelly-sands, little or no fines.
  • Allowable bearing capacity in pounds per square foot with medium compaction or stiffness: 5000.
  • Drainage Characteristics: Good.
  • Frost heave potential: Low.
  • Volume change potential: Low.

GM

  • Silty-gravels, gravel-sand-silt mixtures.
  • Allowable bearing capacity in pounds per square foot with medium compaction or stiffness: 4000.
  • Drainage Characteristics: Good.
  • Frost heave potential: Medium.
  • Volume change potential: Low.

SM

  • Silty-sand, sand-silt mixtures.
  • Allowable bearing capacity in pounds per square foot with medium compaction or stiffness: 4000.
  • Drainage Characteristics: Good.
  • Frost heave potential: Medium.
  • Volume change potential: Low.

Group II  (Fair to Good)

GC

  • Clayey-gravels, gravel-sand-clay mixtures.
  • Allowable bearing capacity in pounds per square foot with medium compaction or stiffness: 4000.
  • Drainage Characteristics: Good.
  • Frost heave potential: Medium.
  • Volume change potential: Medium.

SC

  • Clayey-sands, sand-clay mixtures.
  • Allowable bearing capacity in pounds per square foot with medium compaction or stiffness: 4000.
  • Drainage Characteristics: Medium.
  • Frost heave potential: Medium.
  • Volume change potential: Low.

ML

  • Inorganic silts and very fine sands, rock flour, silty or clayey fine sands or clayey silts with slight plasticity.
  • Allowable bearing capacity in pounds per square foot with medium compaction or stiffness: 2000.
  • Drainage Characteristics: Medium.
  • Frost heave potential: High.
  • Volume change potential: Low.

CL

  • Inorganic clays of low to medium plasticity, gravelly clays, sandy clays, silty clays, lean clays.
  • Allowable bearing capacity in pounds per square foot with medium compaction or stiffness: 2000.
  • Drainage Characteristics: Medium.
  • Frost heave potential: Medium.
  • Volume change potential: Medium.

Group III  (Poor)

CH

  • Inorganic clays of high plasticity, fat clays.
  • Allowable bearing capacity in pounds per square foot with medium compaction or stiffness: 2000. 
  • Drainage Characteristics: Poor.
  • Frost heave potential: Medium.
  • Volume change potential: High.

MH

  • Inorganic silts, micaceous or diatomaceous fine sandy or silty soils, elastic silts.
  • Allowable bearing capacity in pounds per square foot with medium compaction or stiffness: 2000.
  • Drainage Characteristics: Poor.
  • Frost heave potential: High.
  • Volume change potential: High.

Group IV  (Unsatisfactory)

OL

  • Organic silts and organic silty clays of low plasticity.
  • Allowable bearing capacity in pounds per square foot with medium compaction or stiffness: 400.
  • Drainage Characteristics: Poor.
  • Frost heave potential: Medium.
  • Volume change potential: Medium.

OH

  • Organic clays of medium to high plasticity, organic silts.
  • Allowable bearing capacity in pounds per square foot with medium compaction or stiffness: -0-.
  • Drainage Characteristics: Unsatisfactory.
  • Frost heave potential: Medium.
  • Volume change potential: High.

Pt

  • Peat and other highly organic soils.
  • Allowable bearing capacity in pounds per square foot with medium compaction or stiffness: -0-.
  • Drainage Characteristics: Unsatisfactory.
  • Frost heave potential: Medium.
  • Volume change potential: High.

  As you well know, the gravel is key in the drainage system. It provides an unobstructed path for the water to flow away from the foundation or into a sump in a full-basement. The gravel will, further more, help to prevent pressures from building up against the foundation and curtail deflection.

Comment let me know what you think.  Have a goo day!

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