﻿<?xml version="1.0" encoding="utf-8"?>
<rdf:Description rdf:about="https://catalogues.royalsociety.org:443/CalmView/record/catalog/NLB/52/100" xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:dc="http://purl.org/dc/elements/1.1/">
  <dc:title>Copy letter from Robert William Frederick Harrison, Assistant Secretary of the Royal Society to Robert Jones</dc:title>
  <dc:description>'Your paper on the motion of a stream  of finite deapth past a body has been carefully considered and the Committee to which it was referred are prepared to recommen it for publication, but before proceeding further in the matter I am desired to communicate the following suggestion to you for your consideration, and to ask whether you would care to make a short addition to the paper on the lines suggested in this note:- 
The author should be asked to discuss how far the superposition of a circulation round the body, which is artiificially adjusted so as to avoid a singularity at one edge, is likely  to be a good representation of the action of a viscous eddying strea,. Kutta and others have assumed that this is so, without however really going into the question. It is very [important] that this question should be gone into.'</dc:description>
  <dc:date>12 August 1915</dc:date>
</rdf:Description>