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Earthwork Design

The following information supplements PDDM Section 9.5.1.

While roadway excavation is not classified for measurement or payment purposes, it may be categorized for computation of earthwork design and mass purposes as the following types:

  1. Common Material. Common material is largely earth or earth with detached boulders less than 0.5 cuyd [0.5 m3].
  2. Rippable Rock. Rippable rock refers to material ready for excavating after being loosened by a ripper.
  3. Solid Rock. Solid rock includes hard rock in place, ledge rock and boulders requiring drilling and blasting equipment for removal. Any blasting work will be performed according to the rock blasting section specifications.

Determination of Excavation and Embankment Volumes

Use the average end-area method of determining volumes. The total volume of earthwork is the sum of the volumes of the prismoids formed by adjacent cross sections.

When using the average end-area method, the prismoid is treated as a prism whose cross section is the mean of the two end areas of the prismoid. Equation 9.5.1A(1) presents the formula for use in the average end-area method.

Equation 9.5.1A(1)
V=L(A1+A2)/2

Where:

V = Volume, cubic yard [m3]
A1 and A2 = Cross sectional end areas, square feet [m2]
L = Distance between the cross sections, ft [m]

This formula is approximately correct. Due to its simplicity and substantial accuracy in the majority of cases, it has become the formula in common use. It gives results, in general, larger than the true volume.

When the earthwork center of mass (centroid of the area of cut or fill) is not centered about the roadway, and the alignment is in curvature, the actual volume calculated is not correct since the true distance between the end area centroids will differ from the distance along the centerline. In this case it may be necessary to adjust excavation volumes for curvature in order to properly account for earthwork. In many cases this is not necessary since the eccentricities about centerline of the earthwork mass tend to equalize themselves over the route.

Shrink and Swell Factors

Using data furnished by the Geotechnical Unit, the designer must check the characteristics of the material to be excavated or placed in embankments. The excavation used for embankments will range from rock to earth and have shrink/swell factors assigned for design purposes.

The values shown in Exhibit 5.1 A may be used for estimating purposes prior to obtaining the project specific information from the Geotechnical Unit.

Material Measured
In-Situ
Mass Density1
Loose Embankment
Mass Density2 %
Swell3
Mass Density2 %
Swell3
lb/yd3 kg/m3 lb/yd3 kg/m3 lb/yd3 kg/m3
Andesite 4950 2930 2970 1760 67 3460 2050 43
Basalt 4950 2935 3020 1790 64 3640 2160 36
Bentonite 2700 1600 2000 1185 35      
Breccia 4050 2400 3040 1800 33 3190 1890 27
Calcite-Calcium 4500 2670 2700 1600 67      
Caliche 2430 1440 2100 1245 16 3200 1900 -25
Chalk 4060 2410 2170 1285 50 3050 1810 33
Charcoal     1030 610        
Cinders 1280 760 960 570 33 1420 840 -10
Clay
 Dry
 Damp

3220
3350

1910
1985

2150
2010

1275
1180

50
67

3570
3720

2120
2205

-10
-10
Conglomerate 3720 2205 2800 1660 33      
Decomposed rock
 75%R. 25%E.
 50%R. 50%E.
 25%R. 75%E.

4120
3750
3380

2445
2225
2005

3140
2710
2370

1865
1610
1405

31
38
43

3680
4000
3720

2185
2375
2205

12
-6
-9
Diorite 5220 3095 3130 1855 67 3650 2165 43
Diotomaceous earth 1470 870 910 540 62      
Dolomite 4870 2890 2910 1725 67 3400 2015 43
Earth, loam
 Dry
 Damp
 Wet, mud

3030
3370
2940

1795
2000
1745

2070
2360
2940

1230
1400
1745

50
43
0

3520
3520
3520

2090
2090
2090

-12
-4
-20
Feldspar 4410 2615 2640 1565 67 3080 1825 43
Gabbro 5220 3095 3130 1855 67 3650 2165 43
Gneiss 4550 2700 2720 1615 67 3180 1885 43
Gravel (Dry)
 Uniformly Graded
 Avg. Gradation
 Well Graded

2980
3280
3680

1770
1945
2180

2700
2730
2770

1600
1620
1645

10
20
33

3150
3570
4130

1870
2120
2450

-5
-8
-11
Gravel (Wet)
 Uniformly Graded
 Avg. Gradation
 Well Graded

3310
3640
4090

1965
2160
2425

3150
3290
3520

1870
1950
2090

5
10
16

3150
3570
4130

1870
2120
2450

-5
-2
-1
Granite 4540 2695 2640 1565 72 3170 1880 43
Gumbo
 Dry
 Wet

3230
3350

1915
1985

2150
2020

1275
1200

50
67

3570
3720

2120
2205

-10
-10
Gypsum 4080 2420 2380 1410 72      
Igneous rocks 4710 2795 2820 1675 67 3300 1960 43
Kaolinite
 Dry
 Wet

3230
3350

1915
1985

2150
2010

1275
1190

50
67

 

 

 
Limestone 4380 2600 2690 1595 63 3220 1910 36
Loess
 Dry
 Wet

3220
3350

1910
1985

2150
2010

1275
1190

50
67

3570
3720

2120
2205

-10
-10
Marble 4520 2680 2700 1600 67 3160 1875 43
Marl 3740 2220 2240 1330 67 2620 1555 43
Masonry, rubble 3920 2325 2350 1395 67 2750 1630 43
Mica 4860 2885 2910 1725 67      
Pavement
 Asphalt
 Brick
 Concrete
 Macadam

3240
4050
3960
2840

1920
2400
2350
1685

1940
2430
2370
1700

1150
1440
1405
1010

50
67
67
67

3240
2840
2770
2840

1920
1685
1645
1685

0
43
43
0
Peat 1180 700 890 530 33      
Pumice 1080 640 650 385 67      
Quartz 4360 2585 2610 1550 67 3000 1780 43
Quartzite 4520 2680 2710 1610 67 3160 1875 43
Rhyolite 4050 2400 2420 1435 67 2870 1700 43
Riprap rock 4500 2670 2610 1550 72 3150 1870 43
Sand
 Dry
 Wet

2880
3090

1710
1915

2590
3230

1535
1835

11
5

3240
3460

1920
2050

-11
-11
Sandstone 4070 2415 2520 1495 61 3030 1795 34
Schist 4530 2685 2710 1610 67 3170 1880 43
Shale 4450 2640 2480 1470 79 2990 1775 49
Silt 3240 1920 2380 1410 36 3890 2310 -17
Siltstone 4070 2415 2520 1495 61 4560 2705 -11
Slate 4500 2670 2600 1540 77 3150 1870 43
Talc 4640 2750 2780 1650 67 3250 1930 43
Topsoil 2430 1440 1620 960 56 3280 1945 -26
Tuff 4050 2400 2700 1600 50 3050 1810 33
Footnotes:
  1. Subject to average ±5% variation.
  2. Mass densities are subject to adjustments in accordance with modified swell and shrinkage factors.
  3. Based on average in-situ densities. A negative number represents a shrinkage. Factors subject to ±33% variation.

Roadway excavation is typically measured in the original, undisturbed position. The specifications must clearly state the place and method of measurement because almost all materials change volume in their movement from cut to fill.

Excavated common material will expand beyond its original volume in the transporting vehicle but will typically shrink below the excavated volume when compacted into the fill. To illustrate, 1 cuyd [1 m3] of earth in the cut may use 1.25 cuyd [1.25 m3] of space in the transporting vehicle, and finally occupy only 0.65 to 0.85 cuyd [0.65 to 0.85 m3] in the embankment. This, of course, depends on its original density and the compactive effort applied. This difference between the original volume in a cut and the final volume in a fill is the shrink.

Excavated solid rock placed in a fill typically occupies a larger volume. This change in volume is the swell. When the voids in the rock embankment become filled with earth or other fine material, the volume in the fill will just about equal the combined volumes in the two source locations.

For light soil excavation and for fills constructed on swampy ground subject to settlement, the shrink may range from 20 to 40 percent or even greater. For moderate soil excavation, the shrink ranges from ten to 25 percent. For heavy soil excavation with deep cuts and fills, expect a range of approximately 15 percent shrink to five percent swell. Shrink generally includes the slight waste in transporting material from cut to fill and the loss for material that escapes beyond the toe of slopes. Embankments that are slightly overbuilt also contribute to an apparent shrink.

The underlying soil below embankments may also settle and compact, or be displaced, due to placement and compaction of the embankment, contributing to an apparent shrink. Settlement results in apparent shrinkage, but one is not directly proportional to the other. Do not confuse shrink with subsidence. Subsidence is settlement of the entire embankment due to weak foundation conditions (e.g., placing heavy fill on swampy soil).

A swell of 5 to 25 percent is often anticipated in rock excavation depending upon the proportion of solid rock and upon the size of the rock placed in the fill. Rock blasting, especially cushion blasting, is inexact and may result in slightly over-excavated slopes, contributing to an apparent swell.

When available, the design should consider actual field shrink and swell factors for like material used on adjoining projects.

Balancing Earthwork

It frequently happens that the material from the adjacent cuts is not sufficient to make the intervening fill. In this case, material is borrowed from outside the construction limits.

When there is an excess of excavated material, it may be necessary to dispose of the material. Instead of long hauls, it may be more economical to dispose of the material by widening shoulders or placing the material in disposal areas than to pay hauling costs.

If the earthwork is not in balance, the designer should try to adjust grade line or centerline so it is in balance. When a balanced project is not practical or desirable, the designer either disposes of excess material or borrows material to obtain a balance. Designated disposal or borrow areas require clearance for proper ownership, rights-of-use, environmental concerns and applicable permits.

Waste areas for the disposal of excess material and/or borrow areas should be shown on the plans.

Haul

Haul consists of transporting material from its original position to its final location. The cost to haul material is required to estimate the unit price of various items of work.

Haul costs are based on hauling one cubic yard [cubic meter] of material a distance of 1 mile [1 km] or 1 ton [1 metric ton] of material a distance of 1 mile [1 km] using the shortest practical route. Haul costs are generally based on a rate per unit of time for the hauling equipment multiplied by the actual time needed to move the material. This is quite simple when calculating costs to haul from crusher sites to the middle of a project. It is more complicated to estimate the costs to haul material between balance points on a grading project. The use of a mass diagram as described below will provide the quantity of haul within balance points as well as other helpful information. The haul cost will be much greater for haul in the uphill direction than in the downhill direction.