The Dead Heart of Australia
The Dead Heart of Australia
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In our eReader you can find the full English version of the book. Read The Dead Heart of Australia Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book The Dead Heart of Australia
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36.
1 A. P. Folwell, Water-supply Engineering, 1900, pp. 216, 218.
ISOPOTENTIALS 305 be reduced below a factor, which would be suffi- cient to obliterate the whole of the hydrostatic head from any distant sources.
2. Irregularities in the Distribution of the Water and its Pressure We have already seen that, in a complex artesian basin, the hydraulic gradient will not be a regular uniform slope from the intake to the level of discharge. But when we turn to the distribution of water-pressure in A...ustralia, we find that it is far more irregular, than can be explained by the complexity of the water-bed. It is true that the level to which the water will rise from the wells is greatest at two localities in the Queensland hills, and from these high-pressure areas there is, speaking generally, a fall north-eastward to the Gulf of Carpentaria and south-westward to Lake Eyre. Mr. J. B. Henderson, of Brisbane, has constructed maps with isopotential lines, showing the levels to which the water will rise at various localities, and these look, at first, as if we were dealing with a simple, hydraulic gradient.
What to read after The Dead Heart of Australia?
You can find similar books in the "Read Also" column, or choose other free books by J W John Walter Gregory to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
36.
1 A. P. Folwell, Water-supply Engineering, 1900, pp. 216, 218.
ISOPOTENTIALS 305 be reduced below a factor, which would be suffi- cient to obliterate the whole of the hydrostatic head from any distant sources.
2. Irregularities in the Distribution of the Water and its Pressure We have already seen that, in a complex artesian basin, the hydraulic gradient will not be a regular uniform slope from the intake to the level of discharge. But when we turn to the distribution of water-pressure in A...ustralia, we find that it is far more irregular, than can be explained by the complexity of the water-bed. It is true that the level to which the water will rise from the wells is greatest at two localities in the Queensland hills, and from these high-pressure areas there is, speaking generally, a fall north-eastward to the Gulf of Carpentaria and south-westward to Lake Eyre. Mr. J. B. Henderson, of Brisbane, has constructed maps with isopotential lines, showing the levels to which the water will rise at various localities, and these look, at first, as if we were dealing with a simple, hydraulic gradient.
What to read after The Dead Heart of Australia?
You can find similar books in the "Read Also" column, or choose other free books by J W John Walter Gregory to read onlineMoreLess
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