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  2. Hydraulic roughness - Wikipedia

    en.wikipedia.org/wiki/Hydraulic_roughness

    The value of Manning's n is affected by many variables. Factors like suspended load, sediment grain size, presence of bedrock or boulders in the stream channel, variations in channel width and depth, and overall sinuosity of the stream channel can all affect Manning's n value. For instance, a narrow, rocky channel with irregular obstructions ...

  3. Manning formula - Wikipedia

    en.wikipedia.org/wiki/Manning_formula

    Overbank n values for a given reach will vary greatly depending on the time of year and the velocity of flow. Summer vegetation will typically have a significantly higher n value due to leaves and seasonal vegetation. Research has shown, however, that n values are lower for individual shrubs with leaves than for the shrubs without leaves. [7]

  4. Albert Strickler - Wikipedia

    en.wikipedia.org/wiki/Albert_Strickler

    Strickler’s equation introduces a new emperical coefficient which must be determined experimentally to define n-value. However, unlike n-value, which has units of T/L 1/3, has units of length, and at least in theory, is a measurable quantity. [Notes 1] A measurable quantity is potentially useful for channel design and stream restoration ...

  5. Rosgen Stream Classification - Wikipedia

    en.wikipedia.org/wiki/Rosgen_Stream_Classification

    The Rosgen Stream Classification is a system for natural rivers in which morphological arrangements of stream characteristics are organized into relatively homogeneous stream types. [1] This is a widely used method for classifying streams and rivers based on common patterns of channel morphology. [ 2 ]

  6. Standard penetration test - Wikipedia

    en.wikipedia.org/wiki/Standard_penetration_test

    Symbol used in drawings Standard penetration test N values from a surficial aquifer in south Florida. The standard penetration test (SPT) is an in-situ dynamic penetration test designed to provide information on the geotechnical engineering properties of soil. This test is the most frequently used subsurface exploration drilling test performed ...

  7. Streamflow - Wikipedia

    en.wikipedia.org/wiki/Streamflow

    Streamflow values are better indicators than gage height of conditions along the whole river. Measurements of streamflow are made about every six weeks by United States Geological Survey (USGS) personnel. They wade into the stream to make the measurement or do so from a boat, bridge, or cableway over the stream.

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  9. HEC-RAS - Wikipedia

    en.wikipedia.org/wiki/HEC-RAS

    3D view. HEC-RAS is simulation software used in computational fluid dynamics – specifically, to model the hydraulics of water flow through natural rivers and other channels.. The program was developed by the United States Army Corps of Engineers in order to manage the rivers, harbors, and other public works under their jurisdiction; it has found wide acceptance by many others since its ...