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单词 grade
释义
grade

Mathematics
  • An angular measure which is one‐hundredth of a right angle.


Biology
  • A group of organisms that share certain morphological characteristics but are not necessarily related in evolutionary terms. For example, all organisms that possess a coelom can be regarded as a grade. A grade can be contrasted with a clade, which represents a group comprising an ancestral species and all its descendants.


Geology and Earth Sciences
  • 1. Group of things all of which have the same value.

    2. A balanced condition, especially of a river (river or stream grade) when it has just sufficient energy to transport the load supplied from the drainage basin; a balance between erosion and deposition. The concept has also been applied to hillslopes (‘graded slopes’) that are stable dynamically and so maintain themselves in the most economical configuration. The term is no longer used widely as it oversimplifies the issues involved.

    3. The fraction of a sediment falling within a particular size limit, e.g. sand grade, silt grade, and boulder grade. See particle size.

    4. The quality of a mineral ore.

    5. Classification of an ore by the quantity or purity of the mineable metal in an orebody.

    6. In civil engineering, the gradient of a road.

    7. Distinctive functional or structural level of complexity in the organization of an organism. Thus fish, amphibians, reptiles, and mammals represent successive vertebrate grades. Grades may occur within a single lineage; or the same grade may be achieved independently in different ones (e.g. warm-bloodedness evolved independently in birds and mammals).

    8. See metamorphic grade.


Geography
  • In geomorphology, a state of equilibrium in a system. A river is said to be graded when it can: transport the 1.5 year water discharge within the bankfull channel; transport all grain sizes supplied by the watershed without net erosion or deposition; and balance any bank erosion with an equal amount of bank sedimentation; that is to say that it has sufficient discharge to transport its load, but not enough energy for erosion; if any of the factors controlling discharge changes, the river will react to re-establish grade; see A. S. Goudie and K. A. Gregory (2011) pp. 365–6. Grade over one section of a river course is a graded reach. A graded slope has an angle at which output, throughput, and input remain in equilibrium.


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