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Danbones
reply to post by Harte
it doesan't?
prove it
only this time use links that don't impeach your self
ACOUSTIC PROPERTIES OF LIMESTONES FROM THE NORTH-CENTRAL PACIFIC,
DEEP SEA DRILLING PROJECT LEG 621
www.deepseadrilling.org...
AGAIN from your linkedit on 3-3-2014 by Danbones because: (no reason given)
and again again:
The density-velocity relationship of the carbonates shows excellent correlation with Gardners curve for limestone. The
general Gardners curve, however, underestimates the velocities of the volcaniclastics. Laboratory porosity-velocity trends of the
carbonates are consistently 5% to 20% higher than those predicted by the time-average equation using the correct matrix velocities.
Similar crossplots for the volcaniclastics show a division into two distinct subgroups, each corresponding to a time-average
equation with a different matrix velocity, which suggests that progressive diagenetic alteration of the volcaniclastics has decreased
the matrix velocity. The VjJVs
ratios of the carbonates do not discriminate mineralogic composition. Laboratory measurements,
under effective pressure simulating in situ conditions, are 5% to 25% higher than analyses of velocity made aboard JOIDES
Resolution under atmospheric pressure.
The carbonates at Site 866 have a considerably wider range of acoustic impedance than the basalt. As a consequence, the
contact between the carbonate succession and the underlying basalt basement in many drowned Cretaceous guyots of the equatorial
Pacific Ocean may be difficult to image seismic-reflection profiles
Danbonesdoesn't matter the fundamental frequency...there will be harmonics in pretty much all human defined ranges which are arbitrary and reflect the definitions imposed by scientific disciplines
Sound Absorption Coefficients
Concrete Block – Light, Porous .36 .44 .31 .29 .39 .25
Concrete Block – Dense, Painted .10 .05 .06 .07 .09 .08
Gypsum Board – 1/2″, Nailed to 2×4, 16″ O.C. .29 .10 .05 .04 .07 .09
Marble or Glazed Tile .01 .01 .01 .01 .02 .02
Plaster – Gypsum, or Lime, Smooth Finish on Tile or Brick .013 .015 .02 .03 .04 .05
Plaster – Gypsum, or Lime, Rough Finish on Lath .14 .10 .06 .05 .04 .03
Plaster – Gypsum, or Lime, Smooth Finish on Lath .14 .10 .06 .04 .04 .
However, as another poster pointed out already, the reflection of sound off a stone surface depends almost completely on the smoothness of that surface, and not on what kind of stone is behind the surface.
The terms source, receiver and reflecting interface are introduced. Sound energy travels through different media (rocks) at different velocities and is reflected at interfaces where the media velocity and/or density changes. The amplitude and polarity of the reflection is proportional to the acoustic impedance (product of velocity and density) change across an interface. The arrival of energy at the receiver is termed a seismic event. A seismic trace records the events and is conventionally plotted below the receiver with the time (or depth axis) pointing down the page. Click here to see a movie illustrating wave propagation. The colour background is the velocity field.
Danbones
Sound Absorption Coefficients
www.acousticalsurfaces.com...
geeez
phascepalm
Concrete Block – Light, Porous .36 .44 .31 .29 .39 .25
Concrete Block – Dense, Painted .10 .05 .06 .07 .09 .08
Gypsum Board – 1/2″, Nailed to 2×4, 16″ O.C. .29 .10 .05 .04 .07 .09
Marble or Glazed Tile .01 .01 .01 .01 .02 .02
Plaster – Gypsum, or Lime, Smooth Finish on Tile or Brick .013 .015 .02 .03 .04 .05
Plaster – Gypsum, or Lime, Rough Finish on Lath .14 .10 .06 .05 .04 .03
Plaster – Gypsum, or Lime, Smooth Finish on Lath .14 .10 .06 .04 .04 .
go the link look up what the numbers mean
eta..repitition for emphasis
ABSORPTION COEFFICIENT CHART
www.sae.edu...
everything has an absorbtion /reflection coefficient:
limestone, granite, peanut butter,....even you Harte
Harte
It's quite simple to grasp that stone blocks the transmission of sound, which is what you quoted.
So does granite, sandstone, marble, gneiss, brick and concrete, for that matter.
Harte
Floor materials------------------------125 Hz---250 Hz---500 Hz---1 kHz----2 kHz---4 kHz
Concrete (unpainted, rough finish)---0.01----0.02-----0.04-------0.06------0.08----0.1
Concrete (sealed or painted)---------- 0.01----0.01-----0.02-------0.02------0.02----0.02
Kashigeo PPX Limestone.
Bulk spec. gravity --- 2,48 gr/cm3
Absorption coefficient --- 3,07%
Vicente Beige Limestone.
Bulk specific gravity --- 2,56 gr/cm3
Absorption coefficient --- 1,73
Vicente Blue Limestone.
Bulk spec. gravity --- 2,62 gr/cm3
Absorption coefficient --- 1,80 %
Branco do Mar.
Bulk specific gravity --- 2,36 gr/cm3
Absorption coefficient --- 4,8 %
Danbones
HarteHowever, as another poster pointed out already, the reflection of sound off a stone surface depends almost completely on the smoothness of that surface, and not on what kind of stone is behind the surface.
care to back that up with something a little more substantial then "another poster"?
cause right now you are just talking out your butt
Floor materials------------------------125 Hz---250 Hz---500 Hz---1 kHz----2 kHz---4 kHz
Concrete (unpainted, rough finish)---0.01----0.02-----0.04-------0.06------0.08----0.1
Concrete (sealed or painted)---------- 0.01----0.01-----0.02-------0.02------0.02----0.02
Danbonesdensities of various rocks as per the above little giblet of haha you are wrong Harte
geology.about.com...
Materials
Brick – Unglazed
125Hz 250Hz 500Hz 1000Hz 2000Hz 4000Hz
.03 .03 .03 .04 .05 .07
Brick – Unglazed, Painted
125Hz 250Hz 500Hz 1000Hz 2000Hz 4000Hz
.01 .01 .02 .02 .02 .03
The above is an indication that you are unaware that the density and acoustical properties of stone always vary somewhat,
reflection
Hypothetical Rock Properties
Rock VP, km/s ρ, kg/m3 V x ρ
Granite 5.0 2700 13,500
Basalt 5.5 3000 16,500
Limeston 6.0 2300 13,800
Sandstone 4.2 2500 10,500
Shale 2.5 2300 5,750
Danbones
The above is an indication that you are unaware that the density and acoustical properties of stone always vary somewhat,
lol
what you just illustrated is everything has a different absorption reflection co efficient at the density boundry
which is what i said
reflection
Hypothetical Rock Properties
Rock VP, km/s ρ, kg/m3 V x ρ
Granite 5.0 2700 13,500
Basalt 5.5 3000 16,500
Limeston 6.0 2300 13,800
Sandstone 4.2 2500 10,500
Shale 2.5 2300 5,750
principles.ou.edu...
Danbones
we are done here Harte
What types of surfaces reflect sound the best?
In: Sound Waves [Edit categories]
Answer:
We will find surfaces that are
hard and flat
to be the best reflectors of sound. To understand why, we need to review a couple of things about sound.
Sound is mechanical energy. The source of the sound will put the sound (mechanical) energy into the medium through which that sound is going to travel. This causes some movement in the medium through which the sound is propagating.
Surfaces that reflect sound best will not absorb the sound energy by moving. These surfaces will resist any movement and will thus not take any energy from the sound wave. This said, we'd expect a foam rubber wall will reflect far less sound energy than a concrete wall. Also, a wall that is flat will cause less scattering, which is a distributed redirection of the sound.
A flat wall will allow sound to be reflected directly back toward the source (for sound arriving at a right angle to the wall).
A wall that is made of cemented river stones, which are rounded, will scatter some of the sound energy and be less as good a reflector of that sound compared to a flat, smooth concrete wall.
Granite
A popular choice and becoming a household standard, granite adds both beauty and value to your home. It’s a practical choice because of it’s natural strength, durability, and resistance to both heat and staining. Granite begins to melt around 1215 to 1260°C, so hot pans and pots are no threat and can be placed directly onto the granite countertop.
Granite is a hard rock sitting around a 6 or 7 on Moh’s scale of mineral hardness depending on the exact mix of minerals (quartz, feldspars, micas, and trace amounts of other minerals) making up a specific slab. This property makes granite difficult to scratch. And if scratching does occur, granite is one of the easiest rocks to fix.
Granite comes in literally thousands of colours and has a medium to coarse grain. This means all the different colours from the blend of minerals are easy to see.
Perfect for any room, granite can be used in fireplaces, countertops, bathtubs and showers, indoors, outdoors, and almost anywhere you can imagine.
Limestone
Limestone is a sedimentary rock formed from compressed calcium carbonate. Usually it forms underwater from the bones and shells of sea creatures as well as coral. Because of this, limestone may contain interesting fossils.
Limestone is even softer than marble. Sitting at 3 to 4 on the Mohs scale, simply scraping a copper penny against limestone can scratch its surface. However, scratches aren’t as visible in limestone as they are in marble.
Limestone comes in all sorts of earthy tones, from near-white and yellow-tan to dark grey and black. Like marble, it has a very high melting point making the stone ideal for limestone fireplaces and mantels.
Danbones
reply to post by Harte
just askin if you said it Harte
can't you tell the difference?
pot calling the kettle black imho
The Greeks probably used limestone because it's easy to both find, quarry and shape.
Please elucidate for us the acoustic properties of limestone that are not matched by other stones. And I don't mean the acoustic properties wherein limestone transfers sound waves through a limestone bed. I mean the property you state that it reflects sound better than, say, granite or, say gneiss or any of the various feldspars.
Danbones
The Greeks probably used limestone because it's easy to both find, quarry and shape.
Please elucidate for us the acoustic properties of limestone that are not matched by other stones. And I don't mean the acoustic properties wherein limestone transfers sound waves through a limestone bed. I mean the property you state that it reflects sound better than, say, granite or, say gneiss or any of the various feldspars.
here is the quote Harte
i asked above because i figured you'd clarify
i have more important things to do at this time then prove that oil geoligists exist over and over again
why don't you start a thread on your views Harte instead of fixating on points that have been made over and over again
like from your quote above
BTS plainly quoted the experts opinion of the limestone seats and you just went on and on about absorbtion ( vs reflection) when any engineer would know its a ratio
and again oil geologists use SOUND seismic waves to detect all the different types of rock via that ratio
edit on Monam3b20143America/Chicago35 by Danbones because: (no reason given)edit on Monam3b20143America/Chicago40 by Danbones because: (no reason given)
burntheships
Acoustic properties of limestone
Limestone has particular acoustic properties.
The Greeks chose limestone to line the seats in
their amphitheaters because of its ability to transfer the sound.
Where did they get this information?
dnr.louisiana.gov...
GEOPHYSICAL SURVEYS
Geophysical techniques used for petroleum exploration utilize equipment to measure such things as: electrical currents, gravitational and magnetic anomalies, heat flow, geochemical relationships, and density variations from deep within the earth. Each technique records a different set of characteristics which can be used to locate hydrocarbons beneath the surface of the earth.
Seismic surveys use vibration (induced by an explosive charge or sound generating equipment) to provide a picture of subterranean rock formations at depth, often as deep as 30,000 feet below ground level (BGL). This is accomplished by generating sound waves downward into the earth's crust which reflect off various boundaries between different rock strata. On land, the sound waves are generated by small explosive charges embedded in the ground or by vibrator trucks, sometimes referred to as thumpers which shake the ground with hydraulically driven metal pads. The human ear can barely hear the thump, but the frequency generated penetrates the earth's crust. The echoes are detected by electronic devices called geophones which receive the reflected sound waves and the data are recorded on magnetic tape which is printed to produce a two-dimensional graphic illustrating the subsurface geology.
Offshore surveys are conducted in a slightly different manner. Boats tow cables containing hydrophones in the water, which is similar to geophones on land. Sound waves use to be created by dynamite, but this method killed a variety of sea life. The most acceptable method today is to generate sound waves using pulses of compressed air which creates large bubbles that burst beneath the water surface creating sound. The sound waves travel down to the sea floor, penetrate the rocks beneath, and return to the surface where they are intercepted by the hydrophones. Processing and illustration is the same as the dry land method.
In this type of survey, sound waves are sent into the earth where they are reflected by the different layers of rock. The time taken for them to return to the surface is measured as a function of time. This measurement reveals how deep the reflecting layers are; the greater the time interval, the deeper the rock layer. Moreover, this technique also can determine what type of rock is present because different rocks transmit sound waves differently.
The most sophisticated seismic surveys are three-dimensional (3-D). The recorded data is processed by computer and the results are a detailed, 3-D picture of the formations and structures below the surface. The process is expensive, on the order of $30,000 per mile
In ancient Egyptian art no representations have been found of the sawing of stone by means of a copper blade and an abrasive nor has any lapidary slabing saws been found in the archaeological record (...
from the above link
Early ancient Egyptian lapidary slabbing saws would have been made of copper, either cast or cold-worked until the Middle Kingdom,
Third through Fifth Dynasties
During the earliest period, pyramids were constructed wholly of stone. Locally quarried limestone was the material of choice for the main body of these pyramids, while a higher quality of limestone quarried at Tura (near modern Cairo) was used as the outer casing. Granite, quarried near Aswan, was used to construct some architectural elements, including the portcullis (a type of gate) and the roofs and walls of the burial chamber. Occasionally, granite was used in the outer casing as well, such as in the Pyramid of Menkaure
Granite has a porosity ratio of between 0.4% – 1.5%
Limestone has a porosity ratio of between 0.6% – 31%
Absorption
A stone's level of porosity and permeability will determine how absorbent it is.
I also stated that granite (and any other hard stone - not pumice, for example) reflects sound as well or better than limestone. This fact is attested to in the quote you recently provided, given the hardness of granite vs. limestone.
Danbones
I also stated that granite (and any other hard stone - not pumice, for example) reflects sound as well or better than limestone. This fact is attested to in the quote you recently provided, given the hardness of granite vs. limestone.
Harte, you just admitted there is a difference in sound quality between granite and limestone.
i said the quality of sound is different, between granite and limestone, and i mentioned that limestone was chosen for its sound qualities, quote me if im mistake here but i don't recall ever saying limestone was a better reflecter