Integral theorems for the gradient of a vector field, with a fluid dynamical application

Author:

Lilly Jonathan M.1ORCID,Feske Joel2ORCID,Fox-Kemper Baylor2ORCID,Early Jeffrey J.3ORCID

Affiliation:

1. Planetary Science Institute, Tucson, AZ 85719, USA

2. Department of Earth, Environmental, and Planetary Sciences, Brown University, Providence, RI 02912, USA

3. NorthWest Research Associates, Seattle, WA 98105, USA

Abstract

The familiar divergence and Kelvin–Stokes theorem are generalized by a tensor-valued identity that relates the volume integral of the gradient of a vector field to the integral over the bounding surface of the tensor product of the vector field with the exterior normal. The importance of this long-established yet relatively little-known result is discussed. In flat two-dimensional space, it reduces to a relationship between an integral over an area and that over its bounding curve, combining the two-dimensional divergence and Kelvin–Stokes theorems together with two related theorems involving the strain, as is shown through a decomposition using a suitable tensor basis. A fluid dynamical application to oceanic observations along the trajectory of a moving platform is given. The potential extension of the generalized two-dimensional identity to curved surfaces is considered and is shown not to hold. Finally, the paper includes a substantial background section on tensor analysis, and presents results in both symbolic notation and index notation in order to emphasize the correspondence between these two notational systems.

Funder

Division of Ocean Sciences

Publisher

The Royal Society

Reference78 articles.

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2. Aris R. 1962 Vectors, tensors and the basic equations of fluid mechanics. Mineola, NY: Dover Publications, Inc.

3. Incompressible Flow

4. Kundu PK, Cohen IM, Dowling DR. 2016 Fluid mechanics, 6th edn. San Diego, CA: Elsevier Inc.

5. Ogden RW. 1984 Non-linear elastic deformations. Mineola, NY: E. Horwood.

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