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  2. Cubic ton - Wikipedia

    en.wikipedia.org/wiki/Cubic_ton

    Converting cubic tons (i.e., volumes) to measures of weight presents difficulties because organic materials such as timber vary in density. Approximate volume conversions, based on a timber cubic ton of 40 cubic feet: 1 ton (40 cubic feet) = 1.133 cubic metres; 1 cubic metre = 0.883 cubic tons (35.32 cubic feet)

  3. Cut and fill - Wikipedia

    en.wikipedia.org/wiki/Cut_and_fill

    A simple approach involves defining different earthworks features in a computer program and then adjusting elevations manually to calculate the optimal cut and fill. More sophisticated software is able to automatically balance cut and fill while also considering the materials.

  4. Builder's Old Measurement - Wikipedia

    en.wikipedia.org/wiki/Builder's_Old_Measurement

    At that time a "tun" was a wine container of 252 wine gallons, approx 210 imp gal (955 L) weighing about 2,240 lb (1,020 kg), a weight known today as a long ton or imperial ton. In order to estimate the capacity of a ship in terms of 'tun' for tax purposes, an early formula used in England was:

  5. Hundredweight - Wikipedia

    en.wikipedia.org/wiki/Hundredweight

    A hundredweight (cwt) road sign in Alderney, Bailiwick of Guernsey. The short hundredweight is commonly used as a measurement in the United States in the sale of livestock and some cereal grains [4] and oilseeds, paper, and concrete additives and on some commodities in futures exchanges.

  6. List of conversion factors - Wikipedia

    en.wikipedia.org/wiki/List_of_conversion_factors

    Conversions between units in the metric system are defined by their prefixes (for example, 1 kilogram = 1000 grams, 1 milligram = 0.001 grams) and are thus not listed in this article. Exceptions are made if the unit is commonly known by another name (for example, 1 micron = 10 −6 metre).

  7. Bulk density - Wikipedia

    en.wikipedia.org/wiki/Bulk_density

    The bulk density of soil depends greatly on the mineral make up of soil and the degree of compaction. [3] The density of quartz is around 2.65 g/cm 3 but the (dry) bulk density of a mineral soil is normally about half that density, between 1.0 and 1.6 g/cm 3.