THE THEORY OF PISE

The Swedish scientist, Mr. Karl Ellington, of Nossebro, who is basing a

book on pise (in his own tongue) upon the frail foundation of the

present volume, has, in the course of a letter to the author, made some

exceedingly suggestive "guesses at the truth."

"I am very interested to hear that you are proposing to use an hydraulic

rammer for making blocks. I have thought a good deal about this pressure

business. I am trying to scrutinise the thing from 'the inside,' so to

speak. I am trying to trace out how Nature makes rock. That helps us to

understand pise. Nature made all the stratified rocks out of what was

once fine loose earth and mud. Rivers carried the mud out to sea. Waves

pounded and gnawed the shores and got down some more stuff. The tides

went forth and back and shovelled and levelled at the sea-bottom. Some

more mud on top of that, and a few hundred or thousand feet of the heavy

water on top of that--and Nature's pise was in its making. But why do

these mud particles stick together for ever even after that stratum is

raised up high above the sea and the pressure is discontinued? That is

the counterpoint of the whole problem. What is gravitation? Is it some

form of magnetic or electric energy? We don't know. Do particles of mud

grip and hold each other if they are forced together close enough to be

united by some sort of magnetic or electric energy? Or do the particles

only get a 'mechanical' grip on each other? However that may be, we seem

to know now that we can make them grip by bringing them closely

together. It would seem important, then, that we must bring as much of

particle surfaces together within any given cubic space as we possibly

can; that is, we must have as little of 'holes,' 'empty spaces,' pores

and channels as possible in the mass, in the pressed wall. This, then,

would in turn make it important that plenty of very fine (small)

particles must be present in the mass--and so well distributed among the

coarser particles as to be on hand close by wherever there can be one

more chance for a small particle to fill a little chamber that the

coarser particles would like to bridge over. We can think of how well

Nature was fitted for this work of shuffling over all the particles at

the sea-bottom and under great water pressure till she got every

particle into the niche where it would exactly fit. She used waves,

tides, and gulf streams as shovels and mixers and packers, and the water

above as 'hydraulic rammer.' Looking at the pise matter in this way, it

would appear that both the _mixing_ and the _shuffling_ are of vital

importance. And by 'shuffling' I mean in this connection only that the

smaller and larger particles get a chance to shift over a little during

the process of pressing the earth together to hardness, so that the

pressure may not work only and exclusively in a straight downward

direction, but in a sort of wavy zigzag direction as well--much as when

a street-roller is working the macadam and gravel a little forth and

back at the same time as downward. I have a great respect for old tools

which are the outcome of long-time experience and handed-down wisdom.

I suspect the presence of some of that sort of experience in the rammer

described in your book, p. 59. That tool would do the necessary shifting

while attending to its _main_ intention: hammering the mass solidly

together downwards. Now for your hydraulic rammer--is it advisable to

make it blow or press only in a straight line downward? Maybe there

ought to be two or three kinds of strokes alternating--one stroke with a

rifled or wavy surface under the rammer--and the next stroke with a

_plane_ surface. . . . What sort of witchcraft enters into the effect of

_high frequency blows_ as compared with blows with a little longer

intervals between? Do the strokes create also some 'magnetic' effect in

the pounded earth-mass which helps to fasten the particles to each

other? And does this magnetic charge or friction heat, or whatever it

is, act more promptly if one keeps on 'striking the iron while hot,'

instead of letting the charge 'evaporate' and sneak away between

strokes? Two or three of my hairs are turning grey over these questions

alone. You compliment me by insinuating that I might stumble across some

fruitful idea for the forms or boxes if I speculate a little more on the

key-problem. Well, the thing won't leave me alone, so I have thought out

several foolish variations and rejected them too. But the last one seems

to have a little more vitality, so if it will live till I write my next

letter I will tell you about it. One is so apt to follow the temptation

of 'perfecting' an apparatus--at the cost of getting away from keeping

it cheap, simple--and 'fool-proof.' By this time the idea has grown ripe

in my mind, so that I ought to write out a little book on the pise

problem in Swedish and have it printed before springtime. Something

ought to be done. . . . I have to ask you kindly to permit me to make

use of the data contained in your book. To this I will have to add what

special precautions we must observe as to foundations in a climate like

ours. I intend to treat only the pise method. Cob and chalk methods are

not applicable here, as we have such materials only in a few unimportant

spots."

Mr. Ellington has long been an admirer and a firm friend of England, and

he is good enough to regard his country as indebted to ours for the

introduction of pise-building:

"Let me tell you that the help you are giving me now--not me, but my

nation--will work as an additional bond that draws us more closely

towards each other. . . . Some of our people here have always looked too

much towards the South and too little towards the West."

[Headnote: A Pise-Builder's School]

Cottage Building in Cob, Pisé, Chalk and Clay: A Renaissance (2nd edition) · 第 47 / 74 题