USAF Academy, CO 80840
-Original Message-
From: [EMAIL PROTECTED]
[mailto:[EMAIL PROTECTED]]
Sent: Thursday, October 31, 2002
7:51 PM
To: [EMAIL PROTECTED]
Subject: Re: Heat
In a message dated 10/31/2002
4:54:46 PM Alaskan Standard Time, [EMAIL PROTECTED] writes:
Consid
Heat Transfer Question:
If I understand JHB correctly, he assumes that the the melted water will be
in hydrostatic equilibrium with the surrounding ice.
This is true if:
1) the melt water and ice density are equal
2) there is no way for the water to continually squeeze through the pore
spaces an
kPa or 1920 PSI, assuming ice SG
of 1.0.
Jack
-Original Message-
From: [EMAIL PROTECTED]
[mailto:[EMAIL PROTECTED]]
Sent: Thursday 31 October 2002
20:51
To: [EMAIL PROTECTED]
Subject: Re: Heat
In a message dated 10/31/2002 4:54:46 PM Alaskan Standard
Time, [EMAIL PROTECTED
In a message dated 11/1/2002 12:55:48 AM Alaskan Standard Time, [EMAIL PROTECTED] writes:
The pressure of the ice will be similar to that which the probe would
encounter in a comparably deep layer of liquid water -- actually slightly
less, since ice's density is only 97% that of water. Since Eur
- Original Message -
From: "Leonard DiFrancesco" <[EMAIL PROTECTED]>
To: <[EMAIL PROTECTED]>
Sent: Thursday, October 31, 2002 5:53 PM
Subject: Heat
>
> Consideration of the amount of heat required to melt the ice question:
> In the calculation of the amount of heat required was it consi
In a message dated 10/31/2002 4:54:46 PM Alaskan Standard Time, [EMAIL PROTECTED] writes:
Consideration of the amount of heat required to melt the ice question:
In the calculation of the amount of heat required was it considered that as
the probe descends from the surface the stress increases in
