This situation was chosen for two reasons: (1) that
it was as far as possible removed from any accidental pollution from
the sewer in the street; and (2) that in the centre of the garden it
would theoretically run the greatest chance of fæcal contamination
from the manure used. As the well was sunk solely for experimental
purposes this was essential. The garden is on a river-bank and very
slightly raised above the level of the water. The well is only some 5
ft. deep, and the water stands at a level (which varies very slightly)
of about 3 ft. 6 in. from the bottom. The well is lined throughout
from the very bottom to a point some 15 in. above the ground with
large concrete sewer-pipes 2 ft. 3 in. in diameter, and these pipes
have been carefully cemented at their junctions. Outside the pipes a
circle of cement concrete about 4 in. thick has been run in. It will
thus be evident, the sides being perfectly protected, that no water can
possibly enter this well except through the bottom, all contamination
by lateral soakage through the walls being rendered impossible. The
well is surrounded by an asphalte path about 3 ft. wide and slightly
sloping away from it, and it is encircled by a clipped privet hedge
about 5 ft. high, except at those points where the circle of privet
is cut by the paths. There is a closely fitting cover of oak, which
has an outer casing of lead, and thus all contamination from above is
prevented. The water is drawn off through a 2-in. leaden pipe which
passes through the outer concrete and the concrete lining pipe, the
cut passage for the pipe being carefully closed with cement. The pump
is behind the privet hedge, and is provided with a sink and waste pipe
which takes the overflow some twenty or thirty yards to a neighbouring
stream. In this way the constant dripping of water in the neighbourhood
of the well is prevented; for I am very much alive to the dangers
attending a constant water-drip, which might be able in time to worm
its way through soil and concrete into the well itself. I regard this
question of the overflow as one of great importance which is too often
neglected. Figs. 22 and 23 show this well in section and plan. The
nearest point to the well upon which any manurial deposit of excreta
is likely to be made is on the far side of the privet hedge, and the
distance of this point from the bottom of the well is 7 ft. All water
which finds its way into the well must have passed through at least 6
ft. or 7 ft. of earth, and, of course, the great bulk of the water has
passed through a far greater length. Three chemical analyses of this
water, one by Professor Frankland and two by Dr. Kenwood, testify to
its organic purity, and three bacteriological investigations have given
similar indications of purity. A bacteriological examination of the
water from the river Anton and the well water, made on April 11, 1895,
gave 1,133 growths per cubic centimetre for the river and only 7·5 for
the well.
Public-domain text, read in full here on John Shaqi.
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