The present invention relates to icing conditions detectors or sensors that use temperature sensitive probes, which are connected to sensing circuitry and positioned such that measuring voltage or power characteristics provides information for detecting moisture in a fluid flow, and when combined with an ambient temperature measurement serve to detect icing conditions in the atmosphere.
Emerging regulatory requirements for operating aircraft in icing conditions are being interpreted to require more conservative estimates of sensing icing situations than may be provided with existing ice detectors. Application specific Conditions that conventional accretion based detectors may not be able to detect due to Ludlam Limit effects need to be addressed to meet the new requirements. The ability to detect the existence of icing conditions, rather then actual ice accretion, may therefore be required. “Icing conditions” require the presence of liquid moisture in the airflow, and an air temperature below some selected threshold temperature usually specified to be slightly above freezing.
In its broadest form, a single temperature sensitive probe is deployed in the airstream, and is a heated sensor. The sensor can be self-heated from the power used to excite the sensing element, or a separate heater integral to the probe. Air data information, from other sources which are sufficient to calculate area normalized mass flow rate are needed. The power consumed by the probe to maintain itself at a selected temperature above ambient in dry air is known to have a fixed relationship to mass flow rate calculated from the other air data sources. The air data information is independent of the presence of moisture, but, moisture in the air will increase the power drawn by the heated probe relative to the dry condition to maintain the selected temperature. Thus, if the power drawn by the probe deviates from the expected dry air relationship, the presence of moisture is indicated. A measurement of temperature of the ambient air is also needed to determine whether icing conditions are present.
This ability to obtain information relating to the power drawn to provide heat to maintain the probe temperature to indicate the presence of icing conditions is also achieved by providing two identical heated temperature sensors or probes at different locations in substantially the same mass airflow, but where liquid water is removed from the airflow at one location. As shown in
As shown, a flow housing similar to that used with some total air temperature sensors may be used to provide inertial separation between flow channel branches. A heated or self-heated temperature probe that is in the moisture carrying channel branch will respond differently from a similarly heated temperature probe in the channel that is free of moisture, assuming there is moisture present in the free stream airflow. Assuming the probes are maintained at a fixed temperature, in non-moisture or dry air flow there will be increasing amounts of heat removed from each probe as flow rate increases, but the amount of heat removed from each will be substantially the same.
By connecting the two resistance type probes into a bridge, the bridge output voltage will remain near zero and independent of flow rate or air speed in dry air, but if there is liquid moisture present the heat removed from one of the probes, where removal of heat is enhanced by evaporation and/or blow off of warmed water, will cause a temperature change at that probe and therefore a resistance change if the probe is a resistance type temperature sensor. The offset in voltage would be expected to increase with increasing liquid water content. When an ambient air temperature measurement, that is the temperature of the freestream airflow, is provided from a separate source, a determination of icing conditions can be made. Alternately, a temperature probe may be located in one of the flow channels, preferably that from which moisture has been removed, to approximate the freestream air temperature.
If a resistance temperature probe is used, this approach can be modified by including this probe in a bridge circuit. In this modified approach it is not necessary that mass airflow through each channel be substantially equal. By measuring suitable combinations of voltages, the presence of moisture in the branch carrying liquid moisture from the freestream airflow can be determined because the relationships between the measurements will differ compared to conditions when the free stream flow is dry. Temperature can be determined by measuring the voltage drop across the temperature sensor.
Again, the presence of liquid moisture and an air temperature below a threshold, usually slightly above freezing, is required for icing conditions, and these parameters can be provided by the instrument of the present invention.
In
Liquid water is represented by the dashed lines 28, and the flow housing 12 provides inertial separation of the liquid moisture so that little of the liquid water passes into the branch flow channel 26. The branch flow channel 26 has an exhaust opening 30 at its rear or downstream side. This type of a flow housing is used in various temperature sensors, and for example is of the type shown in U.S. Pat. No. 2,970,475 for a gas temperature probe.
In the present invention, the flow housing 12 mounts temperature sensing probes for determining presence of icing conditions, and in this form of the invention, a probe indicated at 34 is mounted in the branch flow channel 27 of flow tube 16, so that the freestream liquid moisture laden air impinges on the probe 34. Any liquid moisture impinging on the probe 34 will affect the power needed for heating or self-heating the probe, assuming it is desired to maintain the probe at constant temperature.
A second temperature sensing probe 38 is mounted in the branch flow channel 26, the flow in which branch channel is essentially free of liquid water, so the airflow across probe 38 is and remains substantially the same as dry, non-liquid water carrying air.
Since the detector must operate in icing environments the detector housing is provided with heaters 35, preferably electrical, to prevent ice build-up. Heaters 35, for example, may be routed internally within the walls of the housing 12 or applied as a mat in a fashion similar to that currently done with many devices that must be ice protected such as temperature probes, pressure probes and antennae.
To prevent deicing heat from significantly influencing the probes within the housing 12, the flow tube, 16, is provided with a number of small holes or perforations 36, to bleed off the heated boundary layer that forms at the inside walls. This technique is currently used in some aircraft total temperature sensors for the same purpose.
A baffle or heat shield 37, is positioned in flow channel 26, to further minimize the influence of deicing heaters located in the forward walls of strut 14, or probe(s) located within flow channel 26. An orifice, 39, provides venting between the baffle 37 and the inner surface of the forward wall of the strut to prevent excessive temperature rise of the baffle wall.
As shown in
The voltage source 46, designated Vsupply, excites the bridge. The output of the bridge is across the opposite terminals from the input, and is designated Vb in
When moisture is such as that indicated by the lines 28 in flow channels 18 and 27 in
As an alternative to self-heating, separate heater elements integral with, or in close proximity to, the temperature sensing elements in the probes 34 and 38 can be used. The mass flow rate of flow stream in the branch channels 26 and 27 is controlled by regulating the size of outlets 22 and 30, as well as the size of opening 24 so that the mass flow is substantially the same over each of the probes 34 and 38.
In a non-moisture situation, there will be more heat removed from each probe as the flow rate increases, but the amount of heat removed from each will be substantially the same. The bridge 40 will remain substantially balanced. Thus, the output voltage designated Vb is independent of the flow rate or air speed.
If, however, there is liquid moisture present in the freestream airflow in branch channel 27, the heat removed from the probe 3A (P1) is enhanced by evaporation and/or blow-off of warmed water since the probes are maintained at a temperature significantly above ambient. This results in a probe temperature change at probe 34 and a resistance change in the probe, and consequently an offset or change in output signal voltage Vb. The offset in Vb increases with increasing liquid water content at the same mass flow of air. There is sensitivity to frozen precipitation such as snow and ice crystals but this sensitivity will be relatively low, and will appear in the form of output voltage spikes that can be filtered by signal conditioning prior to providing the output signal to computer 50, or filtering can be done in the computer 50.
The temperature measurement from the temperature sensor or signal source 54 is combined with the output of the bridge 40, so that the computer provides an output that indicates icing conditions. Icing conditions are indicated when the temperature T is slightly above freezing or less, and when a voltage output from the bridge circuit 40, is caused by liquid moisture being present in branch channel 27 and impinging on probe 34.
In
The resistance element in probe P3 is in the leg of a bridge circuit 64 that is shared by heated probes P1 and P2, as shown in
The arrangement of
Voltage source Vsupply and voltage V3 shown in
It is to be noted that any type of inertial separation flow path can be utilized, and the structure shown herein is merely an example of the type that could be used. The change in direction of a flow can be caused by baffles, obstructions such as posts that cause diversion of particles, and various other shapes and forms of channels that have flow paths branching at a sufficient angle such that the heavier particles will continue in their flow direction under inertial forces and the branch path or bleed path will carry airflow that is substantially free of any liquid moisture particles.
The ability to provide orifices or other flow controls such as the outlets 22 and 30 in
In
In
A probe indicated at 92 and which can be represented as P4 is a heated, or self-heated temperature sensitive probe that is deployed in the airstream, and there is no special ducting required. A flow housing for providing ducting is preferred particularly to control airflow over the probe, to minimize probe operating power and to protect the probe, although the probe can protrude directly into an airstream so long as the liquid water is not separated from the airstream in which the probe is mounted.
In this form of icing conditions detector, the operation of the probe 92 is based upon the well known fact that power consumed by a heated body maintained at a constant temperature above ambient of the airstream is a function of the mass flow rate. It is desired to maintain the body, in this case the probe 92, at a fixed temperature above ambient. Power consumed in a dry environment will have a fixed relationship to the mass flow rate calculated from the air data information available from another source.
Probe 92, which again is self-heated or with a separate heater that is shown schematically at 92H in
In order to provide the data or information necessary to determine the mass flow rate, a pitot (total) pressure input 104, a total air temperature input 106, and a static pressure input 108 can be used to calculate the mass flow rate, and provide the known parameters to the computer 96 for determining the power that would be consumed at the existing mass flow rate if the probe 92 is in dry air. Then, using the actual power consumed from the indicator 100, the computer provides an indication when moisture is present in the airflow. The amount of moisture can also be determined by empirical tests, or calculations that are related to the particular probe 92, and what power this probe consumes or requires to maintain a selected temperature in airflow having liquid moisture conditions at different mass flow measurement rates.
Again, to assess icing conditions, a measurement of temperature from a temperature sensor 106, providing a temperature parameter to a computer system is necessary. Temperature sensing is well known in aircraft, and air data sensors.
The effect of water vapor, that is, humidity, in the airflow will have little influence on performance of the detector of the present invention. The detectors are very sensitive, however, to the presence of water droplets, that is liquid water in the air. It is also recognized that the heat transfer capability of air is not only a function of mass flow rate, but also temperature. Compensating for temperature, if necessary, can be done by suitable analytical techniques that would provide information to a control computer, or direct compensation in the circuitry by having temperature dependent circuit elements. The ability to provide these compensation techniques are presently done in existing mass flow measurement products.
Although the present invention has been described with reference to preferred embodiments, workers skilled in the art will recognize that changes may be made in form and detail without departing from the spirit and scope of the invention.
The present application is a divisional of and claims priority of divisional application Ser. No. 12/174,957 filed Jul. 17, 2008, which is a divisional of and claims priority of divisional U.S. patent application Ser. No. 11/316,187 filed Dec. 22, 2005 (now U.S. Pat. No. 7,416,329), which is a divisional of parent U.S. patent application Ser. No. 10/299,207 filed Nov. 19, 2002 (now U.S. Pat. No. 7,014,357).
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Number | Date | Country | |
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Parent | 12174957 | Jul 2008 | US |
Child | 12691370 | US | |
Parent | 11316187 | Dec 2005 | US |
Child | 12174957 | US | |
Parent | 10299207 | Nov 2002 | US |
Child | 11316187 | US |