BACKGROUND OF THE INVENTION
Field of the Invention
[0001] The present invention relates to a method of controlling nucleation during the freezing
step of a freeze drying cycle and, more particularity, to such a method that uses
a pressure differential ice fog distribution to trigger a spontaneous nucleation among
all vials in a freeze drying apparatus at a predetermined nucleation temperature.
Description of the Background Art
[0002] Controlling the generally random process of nucleation in the freezing stage of a
lyophilization or freeze-drying process to both decrease processing time necessary
to complete freeze-drying and to increase the product uniformity from vial-to-vial
in the finished product would be highly desirable in the art. In a typical pharmaceutical
freeze-drying process, multiple vials containing a common aqueous solution are placed
on shelves that are cooled, generally at a controlled rate, to low temperatures. The
aqueous solution in each vial is cooled below the thermodynamic freezing temperature
of the solution and remains in a sub-cooled metastable liquid state until nucleation
occurs. The range of nucleation temperatures across the vials is distributed randomly
between a temperature near the thermodynamic freezing temperature and some value significantly
(e.g., up to about 30°C.) lower than the thermodynamic freezing temperature. This
distribution of nucleation temperatures causes vial-to-vial variation in ice crystal
structure and ultimately the physical properties of the lyophilized product. Furthermore,
the drying stage of the freeze- drying process must be excessively long to accommodate
the range of ice crystal sizes and structures produced by the natural stochastic nucleation
phenomenon. Nucleation is the onset of a phase transition in a small region of a material.
For example, the phase transition can be the formation of a crystal from a liquid.
The crystallization process (i.e., formation of solid crystals from a solution) often
associated with freezing of a solution starts with a nucleation event followed by
crystal growth.
[0003] Ice crystals can themselves act as nucleating agents for ice formation in sub-cooled
aqueous solutions. In the known "ice fog" method, a humid freeze- dryer is filled
with a cold gas to produce a vapor suspension of small ice particles. The ice particles
are transported into the vials and initiate nucleation when they contact the fluid
interface.
[0004] The currently used "ice fog" methods do not control the nucleation of multiple vials
simultaneously at a controlled time and temperature. In other words, the nucleation
event does not occur concurrently or instantaneously within all vials upon introduction
of the cold vapor into the freeze-dryer. The ice crystals will take some time to work
their way into each of the vials to initiate nucleation, and transport times are likely
to be different for vials in different locations within the freeze-dryer. For large
scale industrial freeze-dryers, implementation of the "ice fog" method would require
system design changes as internal convection devices may be required to assist a more
uniform distribution of the "ice fog" throughout the freeze-dryer. When the freeze-dryer
shelves are continually cooled, the time difference between when the first vial freezes
and the last vial freezes will create a temperature difference between the vials,
which will increase the vial-to- vial non-uniformity in freeze-dried products.
[0005] A need has arisen, therefore, for a method that can produce more rapid and uniform
freezing of the aqueous solution in all vials in a freeze drying apparatus. The method
of the present invention meets this need.
BRIEF SUMMARY OF THE INVENTION
[0006] The invention is defined by the method according to claim 1.
[0007] In the new and improved method of the present invention, an ice fog is not formed
inside the product chamber by the introduction of a cold gas, e.g., liquid nitrogen
chilled gas at -196°C, which utilizes the humidity inside the product chamber to produce
the suspension of small ice particles in accordance with known methods in the prior
art. These known methods have resulted in increased nucleation time, reduced uniformity
of the product in different vials in a freeze drying apparatus, and increased expense
and complexity because of the required nitrogen gas chilling apparatus.
[0008] My related invention disclosed in pending Patent Application Serial No.
13/097,219 filed on April 29, 2012 utilizes the pressure differential between the product chamber and a condenser chamber
to instantly distribute ice nucleation seeding to trigger controlled ice nucleation
in the freeze dryer product chamber. The nucleation seeding is generated in the condenser
chamber by injecting moisture into the cold condenser. The moisture is injected by
releasing vacuum and injecting the moisture into the air entering the condenser. The
injected moisture freezes into tiny suspended ice crystals (ice fog) in the condenser
chamber. The condenser pressure is close to atmosphere, while the product chamber
is at a reduced pressure. With the opening of an isolation valve between the chambers,
the nucleation seeding in the condenser is injected into the product chamber within
several seconds. The nucleation seeding evenly distributes among the super cooled
product triggering controlled ice nucleation.
[0009] It has now been determined that during the opening of the isolation valve the sudden
change of pressure creates strong gas turbulence in the condenser chamber. This turbulence
is capable of knocking off any loosely condensed frost on the condensing surface and
breaks it into larger ice crystals. The larger ice crystals break away from the condensing
surface and mix in the gas flow rushing into the product chamber. The larger size
of the ice crystals enables them to last longer in the product chamber and to make
them more effective in the nucleation process.
[0010] The larger ice crystals help to achieve consistent nucleation coverage and greatly
improve controlled nucleation performance, especially when the product chamber has
restriction in gas flow. such as side plates or when the vapor port is located under
or above the shelf stack. Previously the volume of suspended ice fog in gas form was
limited by the condenser volume. By adding dense frost on the condensing surface,
the physical volume of the condenser is no longer a limitation. The thickness of frost
can easily be controlled to achieve a desired density of larger ice crystals in the
product chamber during nucleation. The condensed frost method works with any condensing
surface. In addition, the size of the condensing chamber may be reduced to increase
the velocity of the gas in the condenser.
BRIEF DESCRIPTION OF THE DRAWINGS
[0011]
FIGURE 1 is a schematic view of one embodiment of apparatus for performing the method
of the present invention;
FIGURE 2 is a schematic view of a second embodiment of apparatus for performing the
method of the present invention connected to a freeze dryer with an internal condenser;
and
FIGURE 3 is a schematic view of the second embodiment of the apparatus for performing
the method of the present invention connected to a freeze dryer having an external
condenser.
DETAILED DESCRIPTION OF THE INVENTION
[0012] As shown in Figure 1, an apparatus 10 for performing the method of the present invention
comprises a freeze dryer 12 having one or more shelves 14 for supporting vials of
product to be freeze dried. A condenser chamber 16 is connected to the freeze dryer
12 by a vapor port 18 having an isolation valve 20 of any suitable construction between
the condenser chamber 16 and the freeze dryer 12. Preferably, the isolation valve
20 is constructed to seal vacuum both ways.
[0013] A vacuum pump 22 is connected to the condenser chamber 16 with a valve 21 therebetween
of any suitable construction. The condenser chamber 16 has a fill valve 24 and a vent
valve 27 and filter 28 of any suitable construction and the freeze dryer 12 has a
control valve 25 and release valve 26 of any suitable construction.
[0014] As an illustrative example, the operation of the apparatus 10 in accordance with
one embodiment of the method of the present invention is as follows:
- 1. Cool down the shelf or shelves 14 to a pre-selected temperature (for example -5°C)
for nucleation below the freezing point of water enough to super cool the product.
- 2. Hold the shelf temperature until all of the product probe temperatures are getting
very close to the shelf temperature (for example within 0.5°C).
- 3. Hold another 10 to 20 minutes for better temperature uniformity across all vials
(not shown).
- 4. With the isolation valve 20 open, open the valve 21 and turn on the vacuum pump
22 to pump down the pressure of the chamber 13 in the freeze dryer 12 and the condenser
chamber 16 to a low point which is still above the vapor pressure of water at the
product temperature to prevent any bubble formation.(for example 50 Torr)
- 5. Close the isolation valve 20 between the product chamber 13 and condenser chamber
16, and close the valve 21.
- 6. Verify condenser temperature is already at its max low usually -53°C or -85°C.
- 7. Open the fill valve 24 to slowly fill the condenser chamber 16 with moisturized
back fill gas up to a predetermined pressure to form a condensed frost of a desired
thickness on the inner surface of the condenser chamber.
- a. The actual gas type and moisture added to the condenser chamber 16 can vary depending
on user preference such that there is sufficient moisture content to generate the
condensed frost, and is within the knowledge of one skilled in the art. As an illustrative
example, the gas and moisture content added to the condenser chamber 16 may be nitrogen
or argon with a sufficient amount of moisture added.
- b. Nozzles, heaters and steam (not shown), for example, may be used as sources of
moisture. Also, moisture may be added to the condenser chamber 16 while in a vacuum.
The vacuum is then released in the condenser chamber 16 to create a pressure differential
with the product chamber 13. As an illustrative example, moisture may be added to
the condenser chamber 16 while under a high vacuum (e.g. 1000 mT) and then the pressure
may be slowly increased in the condenser chamber 16 until it is above the pressure
in the product chamber 13.
- c. Alternatively, moisture may be added to the condenser chamber while it is under
atmospheric pressure or another predetermined pressure that is greater than the pressure
(e.g. 50 Torr-300 Torr) in the product chamber.
- 8. Close the fill valve 24 on the condenser chamber 16.
- 9. Open the vent valve 27 to increase the pressure in the condenser chamber 16.
- 10. Open the isolation valve 20 between the product chamber 13 (at low pressure) and
the condenser chamber 16 (at a higher pressure with condensed frost on the inner surface
thereof).
- a. The sudden change of pressure creates strong gas turbulence in the condenser chamber
which serves to knock off loosely condensed frost on the inner surface thereof and
break it into relatively large ice crystals that mix in the gas flow rushing into
the product chamber to increase the effectiveness of the nucleation process in the
product chamber. The ice crystals are rapidly injected into the product chamber 13
where they are distributed evenly across the chamber and into all of the vials. The
ice crystals serve as nucleation sites for the ice crystals to grow in the sub-cooled
solution. With the even distribution, all of the vials nucleate within a short period
of time.
The nucleation process of all vials will start from top down and finish within a few
seconds.
- b. Also, it is possible to equalize the product chamber pressure and the condenser
chamber pressure at a reduced pressure (e.g., 50 Torr-300 Torr) after the moisture
is added to the condenser chamber under a vacuum, and then open the relief or vent
valve 27 on the condenser to increase the pressure in the condenser chamber 16 and
inject ice crystals into the product chamber 13.
[0015] Figure 2 illustrates a compact condenser 100 connected to a freeze dryer 102 having
an internal condenser 104 which is not constructed to produce condensed frost therein
and requires an additional seeding chamber and related hardware to be added. The freeze
dryer 102 comprises a product chamber 106 with shelves 108 therein for supporting
the product to be freeze dried.
[0016] The compact condenser 100 comprises a nucleation seeding generation chamber 110 having
a cold surface or surfaces 112 defining frost condensing surfaces. The cold surface
112 may be a coil, plate, wall or any suitable shape to provide a large amount of
frost condensing surface in the nucleation seeding generation chamber 110 of the compact
condenser 100. A moisture injection nozzle 1 14 extends into the nucleation seeding
generation chamber 1 10 and is provided with a moisture injection or fill valve 116.
A venting gas supply line 118 having a filter 120 is connected to the nucleation seeding
generation chamber 1 10 by a vacuum release or vent valve 122. The nucleation seeding
generation chamber 110 of the compact condenser 100 is connected to the freeze dryer
102 by a nucleation valve 124.
[0017] In operation, the flow of gas and moisture into the nucleation seeding generation
chamber 110 produces condensed frost on the surfaces of the concentric coils, plates,
walls or other surfaces 112. Since the pressure in the compact condenser 100 is greater
than that in the freeze dryer 102, when the nucleation valve 124 and vent valve 122
are opened, strong gas turbulence is created in the nucleation seeding generation
chamber 110 to remove loosely condensed frost on the inner surfaces of the coils,
plates, walls or other surfaces 112 therein and to break it into ice crystals that
mix in the gas flow rushing into the product chamber 106 to increase the effectiveness
of the nucleation process in the product chamber.
[0018] Figure 3 illustrates a compact condenser 200 connected to a freeze dryer 202 having
an external condenser 204. The construction and operation of the compact condenser
200 is the same as that of the compact condenser 100 shown in Figure 2.
[0019] This method of nucleation is unique by combining an external controllable pre-formation
of condensed frost with a sudden pressure differential distribution method. This results
in a rapid nucleation event because of the large ice crystals, taking seconds instead
of minutes, no matter what size of system it is used on. It gives the user precise
control of the time and temperature of nucleation and has the following additional
advantages:
- 1. Pre-formation of condensed frost in the external condenser chamber is controllable
to allow the formation of the ice crystals to be easily controlled.
- 2. The pressure differential ratio can also be controlled to optimize the distribution
of ice crystals uniformly across all vials within a few seconds.
- 3. No local or batch wise temperature change to the product before the actual nucleation
allows for precise control of nucleation temperature.
- 4. The product chamber will remain in a negative pressure, even after introduction
of the ice crystals. There is no danger of creating a positive pressure.
- 5. This method can be used on any size freeze dryer with an external condenser and
an isolation valve without any system modification. Other methods require significant
modification or cost.
- 6. This method can guarantee the sealed sterile operation mode for pharmaceutical
production environment application.
- 7. The advantage of a uniform nucleation method for the application of freeze drying
is a uniform crystal structure and large aligned crystals across all of the vials,
thus enabling a reduced primary drying process.
- 8. The formation of condensed frost on the inner surface of the condenser chamber
enables a smaller condenser chamber with a high condensing surface area to be used
and added to any freeze dryer. The condensed frost takes up less volume than a suspended
ice fog.
- 9. Compared to the gas form of suspended ice fog, which must be generated just before
the trigger of nucleation, the condensed frost is more stable and can be stored for
an extended period of time and used on demand.
- 10. The frost formation environment can be carefully controlled to generate a loosely
condensed frost which breaks down into ice crystals by gas turbulence during pressure
release by use of a high condenser chamber pressure (e.g., 500 Torr a high volume
low velocity gas flow and a warmer condensing surface temperature (e.g., below 0 degrees
C).
- 11. The larger ice crystals from the condensed frost are denser and stay frozen longer
than the gas form of ice fog during the introduction into the product chamber to expedite
the nucleation process.
- 12. A more compact condenser can be added to systems that don't have an external condenser
or where the existing condenser does not enable building condensed frost, or the existing
condenser can't be validated for sterility. The condenser can be added to an existing
port of sufficient size or by changing the chamber door, for example.
[0020] From the foregoing description, it will be readily seen that the novel method of
the present invention produces a condensed frost in a condenser chamber external to
the product chamber in a freeze dryer and then, as a result of gas turbulence, rapidly
introduces ice crystals into the product chamber which is at a pressure lower than
the pressure in the condenser chamber. This method produces rapid and uniform nucleation
of the product in different vials of the freeze dryer.
1. A method of controlling and enhancing the nucleation of product in a freeze dryer,
comprising:
maintaining the product at a predetermined temperature and pressure in a chamber of
the freeze dryer;
creating a predetermined volume of condensed frost on an inner surface of a condensing
chamber separate from the product chamber; and
when the pressure in the condensing chamber is increased to a predetermined pressure
that is greater than that of the product chamber, creating gas turbulence that breaks
down the condensed frost into ice crystals that rapidly enter the product chamber
for even distribution therein to create uniform and rapid nucleation of the product
in different areas of the product chamber.
2. The method of claim 1 wherein the condensing chamber is connected with the product
chamber by a vapor port.
3. The method of claim 2 wherein the gas turbulence is created by opening the vapor port
into the product chamber when the condensing chamber has the predetermined pressure.
4. The method of claim 2 wherein the vapor port having an isolation valve between the
product chamber and the condensing chamber to open or close vapor flow therebetween.
5. The method of claim 4 wherein a vacuum pump is connected to the condensing chamber
for reducing the pressure within the product chamber and the condensing chamber.
6. The method of claim 2 wherein the pressure within the product chamber is about 50
Torr and the pressure within the condensing chamber is about atmospheric when the
vapor port is opened into the product chamber.
7. The method of claim 1 wherein the temperature of the product is about -5.0°C and the
temperature of the condensing chamber is less than 0°C.
8. The method of claim 1 wherein a predetermined moisturized back fill gas is introduced
into the condensing chamber to produce the condensed frost.
9. The method of claim 8 wherein the moisturized gas is introduced into the condensing
chamber while it is at atmospheric pressure or another predetermined pressure greater
than the pressure in the product chamber.
10. The method of claim 9 wherein the pressure of the condensing chamber is increased
by opening a vent valve on the condensing chamber.
11. The method of claim 8 wherein the moisturized gas is introduced into the condensing
chamber while it is in a vacuum, and the vacuum is thereafter released in the condensing
chamber and its pressure is increased to a pressure greater than the pressure in the
product chamber.
12. The method of claim 11 wherein the vacuum is released using a vent valve on the condensing
chamber while a vapor port between the condensing chamber and product chamber is open,
to create turbulence to drive the ice crystals into the product chamber.
13. The method of claim 11 wherein the vacuum is released in the condensing chamber while
a vent valve on the condensing chamber is open and a vapor port between the condensing
chamber and product chamber is closed, and the ice crystal is driven into the product
chamber by opening the vapor port after the vacuum is released in the condensing chamber.
14. The method of claim 8 wherein the condensing chamber has a fill valve which is opened
to enable the moisturized back fill gas to be introduced into the condensing chamber
to produce the condensed frost, the back fill gas is filtered ambient atmospheric
air and has a moisture content of about 50-80% by volume, and the back fill gas is
nitrogen or argon with moisture added thereto.
15. The method of claim 1 wherein the inner surface of the condensing chamber is defined
by a plurality of inner coils, plates or walls, the inner walls being in a coil configuration
to maximize the size of the inner surface.