This application claims priority under 35 U.S.C. § 119 to Korean Patent Application No. 10-2018-0171137 filed on Dec. 27, 2018 in the Korean Intellectual Property Office, the disclosure of which is hereby incorporated by reference in its entirety.
Example embodiments of the present disclosure relate to methods for nondestructive measurements of a thickness of underlying layers, and, more specifically, to methods for measuring a thickness of underlying layers based on picoseconds ultrasonic measurement methods.
Picoseconds ultrasonic measurement is a type of nondestructive measurement method. Picoseconds ultrasonic measurement methods include generating an ultrasonic wave in a thin layer on a substrate based on using a laser pulse. The ultrasonic wave may change an optical property, including reflectance, for example, of the thin layer. It has been known that a thickness of the thin layer can be measured based on monitoring a variation in the optical property of the thin layer.
According to some example embodiments of the inventive concepts, a method may include irradiating a sample with a pump laser pulse to induce generation of an acoustic wave in the sample such that the acoustic wave propagates through the sample over time, the sample including a substrate, an underlying layer on the substrate, and an overlying layer on the underlying layer, the underlying layer isolated from an exterior of the sample by at least the overlying layer. The method may include irradiating the sample with a probe laser pulse subsequent to irradiating the sample with the pump laser pulse. The method may include determining a reflectance variation of the sample over time, based on monitoring a variation of a reflection of the probe laser pulse from the sample over time, to generate a first graph showing a variation of reflectance of the sample over time, and determining a thickness of the underlying layer based on the first graph.
According to some example embodiments of the inventive concepts, a method may include irradiating a sample with a pump laser pulse to induce generation of an acoustic wave in the sample such that the acoustic wave propagates through the sample over time, the sample including a substrate, an underlying layer on the substrate, an overlying layer on the underlying layer, the underlying layer isolated from an exterior of the sample by at least the overlying layer. The method may include irradiating the sample with a probe laser pulse subsequent to irradiating the sample with the pump laser pulse. The method may include determining a reflectance variation of the sample over time, based on monitoring a variation of a reflection of the probe laser pulse from the sample over time, to generate an initial graph showing a variation of reflectance of the sample over time. The method may include controlling the pump laser pulse and the probe laser pulse based on the initial graph to irradiate the sample with the controlled pump laser pulse and irradiate the sample with the controlled probe laser pulse. The method may include determining the reflectance variation of the sample over time, based on monitoring a variation of a reflection of the controlled probe laser pulse from the sample over time, to generate a final graph showing a variation of reflectance of the sample over time based on the controlling. The method may include determining a thickness of the underlying layer based on the final graph.
According to some example embodiments of the inventive concepts, a method may include generating an acoustic wave in a sample including a substrate, an underlying layer on the substrate, and an overlying layer on the underlying layer, the underlying layer isolated from an exterior of the sample by at least the overlying layer. The method may include generating a first graph showing a reflectance variation of the sample as a function of time during propagation of the acoustic wave in the sample. The method may include determining a thickness of the underlying layer based on the first graph.
Various example embodiments will now be described more fully with reference to the accompanying drawings in which some example embodiments are shown. However, the inventive concepts may be embodied in many alternate forms and should not be construed as limited to only example embodiments set forth herein.
Referring to
The overlying layer 13 may include an arbitrary material and have an arbitrary thickness. In some example embodiments, the overlying layer 13 may include a metal. For example, the overlying layer 13 may include aluminum (Al), tungsten (W), copper (Cu), silver (Ag), gold (Au), but is not limited thereto.
The underlying layer 12 may be disposed between the overlying layer 13 and the substrate 11. The underlying layer 12 may include an arbitrary material and have an arbitrary thickness 12T, which as shown may be a thickness in a direction that is perpendicular to a surface 13S of the overlying layer and/or an incident surface 10S of the sample 10. In some example embodiments, the underlying layer 12 may be formed of the same material as the overlying layer 13 but may be a seed layer having a different density. In some example embodiments, the underlying layer 12 may be formed of a different material form the overlying layer 13. In some example embodiments the underlying layer 12 may be a material formed by reaction of the overlying layer 13 and the substrate 11. For example, the underlying layer 12 may be a silicide layer formed by reaction of metal and silicon. The underlying layer 12 may include a metal, a metal nitride, or a silicide, but is not limited thereto.
Referring to
The pulsed laser 110 may emit a laser beam P. The laser bean P may have any repetition rate, any pulse duration, and any wavelength. For example, the pulsed laser 110 may be a titanium-sapphire laser emitting the laser beam P having the repetition rate of about 10 MHz to 100 MHz, the pulse duration of about 100 fs to 1 ps, and the wavelength of about 400 nm to 800 nm, but is not limited thereto.
The laser beam P may be split into a pump laser bean P1 and a probe laser beam P2. Thereafter, the pump laser beam P1 and the probe laser beam P2 may pass through paths with different lengths and may be incident on the sample 10 (e.g., incident on an incident surface 10S of the sample), such that a probe laser pulse of the probe laser beam P2 arrives at the sample later than a pump laser pulse of the pump laser beam P1. The pump laser beam P1 may be sequentially reflected by a first pump mirror 132, a pump retroreflector 142, and a second pump mirror 133 and may pass through the lens 160, thus being incident on the sample 10. The probe laser beam P1 may be sequentially by a probe retroreflector 141 and a probe mirror 131 and may pass through the lens 160, thus being incident on the sample 10. The length of the path along which the pump laser beam P1 moves may be fixed, whereas the length of the path along which the probe laser beam P2 moves may be adjusted by the delay stage 150. Thus, the sample 10 may be irradiated with a probe laser pulse of the probe laser beam P2 subsequent to being irradiated with a pump laser pulse of the pump laser beam P1, and a time difference between when the pump laser pulse of the pump laser beam P1 arrives at the sample and when the probe laser pulse of the probe laser beam P2 arrives at the sample may be adjusted.
Parts of the pump laser beam P1 and the probe laser beam P2 incident on an incident surface 10S of the sample 10 may be reflected from the incident surface 10S. The incident surface 10S may be, for example, a surface 13S of the overlying layer 13 that is exposed to an exterior of the sample 10 and is distal to the underlying layer 12. The reflected probe laser beam P2 may be detected by a photo detector 170. A reflectance variation of the sample 10 may be measured from the detected reflected probe laser beam P2 by the photo detector 170. The pump laser beam P1 may generate an acoustic wave (e.g., ultrasonic wave) in the sample 10. As the acoustic wave is propagated in the sample 10 over time, the reflectance of the sample 10 for the probe laser beam P2 may be varied over time. Thus, a graph shown in
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The step S200 of irradiating the sample with the probe laser pulse, generating the probe laser beam P2 from the laser beam P by the beam splitter 120, reflecting the probe laser beam P2 by the probe retroreflector 141, reflecting the probe laser beam P2 by the probe mirror 131, passing the probe laser beam P2 through the lens 160, and injecting the probe laser beam P2 into the sample 10 such that the probe laser beam P2 is incident on incident surface 10S of the sample 10 subsequent to the pump laser beam P2 being incident on the incident surface 10S.
The step S300 of measuring the reflectance variation of the sample for the probe laser pulse as the function of time to obtain the graph of time versus reflectance variation may include detecting the probe laser beam P2 reflected from the sample 10 by the photo detector 170, monitoring (“detecting”) variation of the reflection of the probe laser beam P2 from the sample 10 (e.g., from the incident surface 10S) over time, and obtaining the first graph G1 shown in
The step S400 of obtaining (“determining”) the thickness (e.g., 12T) of the underlying layer (e.g., underlying layer 12) from the graph of time versus reflectance variation may include obtaining the thickness of the underlying layer from, (a) reflectance variations at the highest points and the lowest points of the first graph G1, (b) reflectance variations at highest points and lowest points of a second graph obtained by subtracting a saturation value from the first graph G1. (c) reflectance variations at highest points and lowest points of a third graph obtained by removing background noise from the first graph G1, and/or (d) reflectance variations at highest points and lowest points of a fourth graph obtained by normalizing the third graph so that a reflectance variation at a first lowest point of the fourth graph is 0 and a reflectance variation at a first highest point of the fourth graph is 1. Hereinafter, detailed descriptions thereof will be made with reference to
Referring to
For example, when n is 2, the thickness of the underlying layer may be obtained from a difference (ΔR2) between the magnitude of the reflectance variation at the second highest point H2 of the first graph G1 and the magnitude of the reflectance variation at the second lowest point L2 of the first graph G1 and/or a difference (ΔR23) between the magnitude of the reflectance variation at the second highest point H2 of the first graph G1 and the magnitude of the reflectance variation at the third lowest point L3 of the first graph G1.
In some example embodiments, both of the difference (ΔR(Hn)−ΔR(Ln)) between the magnitude of the reflectance variation at the nth highest point of the first graph G1 and the magnitude of the reflectance variation at the nth lowest point of the first graph G1 and the difference (ΔR(Hn)−ΔR(Ln+1)) between the magnitude of the reflectance variation at the nth highest point of the first graph G1 and the magnitude of the reflectance variation at the n+1th lowest point of the first graph G1 may be used to obtain (“determine”) the thickness of the underlying layer of the sample. For example, a sum (i.e., (ΔR(Hn)−ΔR(Ln))+(ΔR(Hn)−ΔR(Ln+1))) of the difference (ΔR(Hn)−ΔR(Ln)) between the reflectance variation at the nth highest point of the first graph G1 and the reflectance variation at the nth lowest point of the first graph G1 and the difference (ΔR(Hn)−ΔR(Ln+1)) between the reflectance variation at the nth highest point of the first graph G1 and the reflectance variation at the n+1th lowest point of the first graph G1 may be used to obtain the thickness of the underlying layer.
In some example embodiments, the thickness of the underlying layer may be obtained from a value from the difference between the magnitude of the reflectance variation at the nth highest point of the first graph G1 and the magnitude of the reflectance variation at the nth lowest point of the first graph G1 to the difference between the magnitude of the reflectance variation at the n+kth highest point of the first graph G1 and the magnitude of the reflectance variation at the n+kth lowest point of the first graph G1, a value from the difference between the magnitude of the reflectance variation at the nth highest point of the first graph G1 and the magnitude of the reflectance variation at the n+1th lowest point of the first graph G1 to the difference between the magnitude of the reflectance variation at the n+kth highest point of the first graph G1 and the magnitude of the reflectance variation at the n+k+1th lowest point of the first graph G1, or any combination thereof. For example, the thickness of the underlying layer may be obtained from a sum (Σi=0i=kΔR(Hn+)−ΔR(Ln+i)) of values, from the difference between the magnitude of the reflectance variation at the nth highest point of the first graph G1 and the magnitude of the reflectance variation at the nth lowest point of the first graph G1 to the difference between the magnitude of the reflectance variation at the n+kth highest point of the first graph G1 and the magnitude of the reflectance variation at the n+kth lowest point of the first graph G1, a sum (Σi=0i=kΔR(Hn+i)−ΔR(Ln+1+i)) of values, from the difference between the magnitude of the reflectance variation at the nth highest point of the first graph G1 and the magnitude of the reflectance variation at the n+1th lowest point of the first graph G1 to the difference between the magnitude of the reflectance variation at the n+kth highest point of the first graph G1 and the magnitude of the reflectance variation at the n+k+1th lowest point of the first graph G1, or any combination thereof. Here, n and k may each be any natural number and may be a common number or different numbers.
For example, when n is 1 and k is 2, the thickness of the underlying layer may be obtained from a sum (i.e., ΔR1+ΔR2+ΔR3) of values, from the difference (ΔR1) between the reflectance variation at the first highest point H1 of the first graph G1 and the reflectance variation at the first lowest point L1 of the first graph G1 to the difference (ΔR3) between the reflectance variation at the third highest point H3 of the first graph G1 and the reflectance variation at the third lowest point L3 of the first graph G1, a sum (i.e., ΔR12+ΔR23+ΔR34) of values, from the difference (ΔR12) between the reflectance variation at the first highest point H1 of the first graph G1 and the reflectance variation at the second lowest point L2 of the first graph G1 to the difference (ΔR34) between the reflectance variation at the third highest point H3 of the first graph G1 and the reflectance variation at a fourth lowest point of the first graph G1, or any combination thereof.
The difference (ΔR(Hn)−ΔR(Ln)) between the reflectance variation at the nth highest point of the first graph G1 and the reflectance variation at the nth lowest point of the first graph G1, the difference (ΔR(Hn)−ΔR(Ln+1)) between the reflectance variation at the nth highest point of the first graph G1 and the reflectance variation at the n+1th lowest point of the first graph G1, the sum (Σi=0i=kΔR(Hn+i)−ΔR(Ln+i)) of values, from the difference between the reflectance variation at the nth highest point of the first graph G1 and the reflectance variation at the nth lowest point of the first graph G1 to the difference between the reflectance variation at the n+kth highest point of the first graph G1 and the reflectance variation at the n+kth lowest point of the first graph G1, and the sum (Σi=0i=kΔR(Hn+i)−ΔR(Ln+1+i)) of values, from the difference between the reflectance variation at the nth highest point of the first graph G1 and the reflectance variation at the n+1th lowest point of the first graph G1 to the difference between the reflectance variation at the n+kth highest point of the first graph G1 and the reflectance variation at the n+k+1th lowest point of the first graph G1 may have correlation with the thickness of the underlying layer. Thus, if the correlation between these values and the thickness of the underlying layer is obtained from experiment, the thickness of the underlying layer may be measured by measuring these values. For example, the greater the thickness of the underlying layer is, the greater these values may be. There may be a linear relationship between the thickness of the underlying layer and these values.
Referring to
For example, the thickness of the underlying layer may be obtained from the magnitude of the reflectance variation (i.e., ΔR(Hn′)) at an nth highest point of the second graph G2, where n is any natural number. When n is 2, the thickness of the underlying layer may be obtained from the magnitude of the reflectance variation (i.e., ΔR2′) at a second highest point H2′ of the second graph G2.
In some example embodiments, the thickness of the underlying layer may be obtained from a value (“magnitude”) from the magnitude of the reflectance variation at the nth highest point of the second graph G2 to the magnitude of the reflectance variation at an n+kth highest point of the second graph G2. For example, the thickness of the underlying layer may be obtained from a sum (i.e., Σi=0i=kΔR(Hn+i′)) of values, from the magnitude of the reflectance variation at the nth highest point of the second graph G2 to the magnitude of the reflectance variation at the n+kth highest point of the second graph G2. Here, n and k may be any natural number. When n is 1 and k is 2, the thickness of the underlying layer may be obtained from a sum (i.e., ΔR1′+ΔR2′+ΔR3′) of values, from the magnitude of the reflectance variation (ΔR1′) at a first highest point H1′ of the second graph G2 to the magnitude of the reflectance variation (ΔR3′) at a third highest point H3′ of the second graph G2.
The reflectance variation (ΔR(Hn′)) at the nth highest point of the second graph G2, the sum (i.e., Σi=0i=kΔR(Hn+i′)) of values, from the reflectance variation at the nth highest point of the second graph G2 to the reflectance variation at the n+kth highest point of the second graph G2, may have correlation with the thickness of the underlying layer. Thus, if the correlation between these values and the thickness of the underlying layer is obtained from experiment, the thickness of the underlying layer may be measured by measuring these values. For example, the greater the thickness of the underlying layer is, the greater these values may be. There may be a linear relationship between the thickness of the underlying layer and these values.
Referring to
The thickness of the underlying layer may be obtained from magnitudes of reflectance values at lowest points (e.g., L″, L2″, L3″) and highest points (e.g., H1″, H2″, H3″) of the third graph G3. For example, the thickness of the underlying layer may be obtained from a difference (ΔR(Hn″)−ΔR(Ln″)) between the magnitude of the reflectance variation at an nth highest point of the third graph G3 and the magnitude of the reflectance variation at an nth lowest point of the third graph G3, a difference (ΔR(Hn″)−ΔR(Ln+1″)) between the magnitude of the reflectance variation at the nth highest point of the third graph G3 and the magnitude of the reflectance variation at an n+1th lowest point of the third graph G3, or any combination thereof. Here, n may be any natural number.
When n is 2, the thickness of the underlying layer may be obtained from a difference (ΔR2″) between the magnitude of the reflectance variation at a second highest point H2″ of the third graph G3 and the magnitude of the reflectance variation at a second lowest point L2″ of the third graph G3 or a difference (ΔR23″) between the magnitude of the reflectance variation at the second highest point H2″ of the third graph G3 and the magnitude of the reflectance variation at a third lowest point L3″ of the third graph G3.
In some example embodiments, the thickness of the underlying layer may be obtained from both of the difference (ΔR(Hn″)−ΔR(Ln″)) between the magnitude of the reflectance variation at the nth highest point of the third graph G3 and the magnitude of the reflectance variation at the nth lowest point of the third graph G3 and the difference (ΔR(Hn″)−ΔR(Ln+1″)) between the magnitude of the reflectance variation at the nth highest point of the third graph G3 and the magnitude of the reflectance variation at the n+1th lowest point of the third graph G3. For example, a sum (i.e., (ΔR(Hn″)−ΔR(Ln″))+(ΔR(Hn″)−ΔR(Ln+1″))) of the difference (ΔR(Hn″)−ΔR(Ln″)) between the reflectance variation at the nth highest point of the third graph G3 and the reflectance variation at the nth lowest point of the third graph G3 and the difference (ΔR(Hn″)−ΔR(Ln+1″)) between the reflectance variation at the nth highest point of the third graph G3 and the reflectance variation at the n+1th lowest point of the third graph G3 may be used to obtain the thickness of the underlying layer.
In some example embodiments, the thickness of the underlying layer may be obtained from a sum of values, from the difference between the magnitude of the reflectance variation at the nth highest point of the third graph G3 and the magnitude of the reflectance variation at the nth lowest point of the third graph G3 to a difference between the magnitude of the reflectance variation at an n+kth highest point of the third graph G3 and the magnitude of the reflectance variation at an n+kth lowest point of the third graph G3, a sum of values, from the difference between the magnitude of the reflectance variation at the nth highest point of the third graph G3 and the magnitude of the reflectance variation at the n+1th lowest point of the third graph G3 to a difference between the magnitude of the reflectance variation at the n+kth highest point of the third graph G3 and the magnitude of the reflectance variation at an n+k+1th lowest point of the third graph G3, or any combination thereof. For example, the thickness of the underlying layer may be obtained from a sum (Σi=0i=kΔR(Hn+i″)−ΔR(Ln+i″)) of values, from the difference between the magnitude of the reflectance variation at the nth highest point of the third graph G3 and the magnitude of the reflectance variation at the nth lowest point of the third graph G3 to the difference between the magnitude of the reflectance variation at the n+kth highest point of the third graph G3 and the magnitude of the reflectance variation at the n+kth lowest point of the third graph G3, a sum (Σi=0i=kΔR(Hn+i″)−ΔR(Ln+1+i″)) of values, from the difference between the magnitude of the reflectance variation at the nth highest point of the third graph G3 and the magnitude of the reflectance variation at the n+1th lowest point of the third graph G3 to the difference between the magnitude of the reflectance variation at the n+kth highest point of the third graph G3 and the magnitude of the reflectance variation at the n+k+1th lowest point of the third graph G3, or any combination thereof. Here, n and k may be any natural number.
For example, when n is 1 and k is 2, a sum (i.e., ΔR1″+ΔR2″+ΔR3″) of values, from a difference (ΔR1″) between the magnitude of the reflectance variation at a first highest point H1″ of the third graph G3 and the magnitude of the reflectance variation at a first lowest point L1″ of the third graph G3 and a difference ((ΔR3″) between the magnitude of the reflectance variation at a third highest point H3″ of the third graph G3 and the magnitude of the reflectance variation at the third lowest point L3″ of the third graph G3 and a sum (i.e., ΔR12″+ΔR23″+ΔR34″) of values from a difference (ΔR12″) between the magnitude of the reflectance variation at the first highest point H1″ of the third graph G3 and the magnitude of the reflectance variation at the second lowest point L2″ of the third graph G3 to a difference ((ΔR34″) between the magnitude of the reflectance variation at the third highest point H3″ of the third graph G3 and the magnitude of the reflectance variation at a fourth lowest point of the third graph G3.
The difference (ΔR(Hn″)−ΔR(Ln″)) between the magnitude of the reflectance variation at the nth highest point of the third graph G3 and the magnitude of the reflectance variation at the nth lowest point of the third graph G3, the difference (ΔR(Hn″)−ΔR(Ln+1″)) between the magnitude of the reflectance variation at the nth highest point of the third graph G3 and the magnitude of the reflectance variation at an n+1th lowest point of the third graph G3, the sum (Σi=0i=kΔR(Hn+i″)−ΔR(Ln+i″)) of values, from the difference between the magnitude of the reflectance variation at the nth highest point of the third graph G3 and the magnitude of the reflectance variation at the nth lowest point of the third graph G3 to the difference between the magnitude of the reflectance variation at the n+kth highest point of the third graph G3 and the magnitude of the reflectance variation at the n+kth lowest point of the third graph G3, and the sum (Σi=0i=kΔR(Hn+i″)−ΔR(Ln+1+i″)) of values, from the difference between the magnitude of the reflectance variation at the nth highest point of the third graph G3 and the magnitude of the reflectance variation at the n+1th lowest point of the third graph G3 to the difference between the magnitude of the reflectance variation at the n+kth highest point of the third graph G3 and the magnitude of the reflectance variation at the n+k+1th lowest point of the third graph G3 may have correlation with the thickness of the underlying layer. Thus, if the correlation between these values and the thickness of the underlying layer is obtained from experiment, the thickness of the underlying layer may be measured by measuring these values. For example, the greater the thickness of the underlying layer is, the greater these values may be. There may be a linear relationship between the thickness of the underlying layer and these values.
Referring to
For example, the thickness of the underlying layer may be obtained from the magnitude of the reflectance variation (i.e., ΔR(Hn+1′″)) at an n+1th highest point of the fourth graph G4, where n is any natural number. For example, when n is 2, the thickness of the underlying layer may be obtained from the magnitude of the reflectance variation (ΔR3′″) at a third highest point H3′″ of the fourth graph G4.
In some example embodiments, the thickness of the underlying layer may be obtained from a value from the magnitude of the reflectance variation at the n+1th highest point of the fourth graph G4 to the magnitude of the reflectance variation at an n+k+1th highest point of the fourth graph G4. For example, the thickness of the underlying layer may be obtained from a sum (i.e., Σi=0i=kΔR(Hn+1+i)) of values, from the magnitude of the reflectance variation at the n+1th highest point of the fourth graph G4 to the magnitude of the reflectance variation at an n+k+1th highest point of the fourth graph G4. Here, n and k may each be any natural number.
For example, when n is 1 and k is 2, the thickness of the underlying layer may be obtained from a sum (i.e., ΔR2′″+ΔR3′″+ΔR4′″) of values, from the magnitude of the reflectance variation (ΔR2′″) at a second highest point H2′″ of the fourth graph G4 to the magnitude of the reflectance variation (ΔR4′″) at a fourth highest point H4′″ of the fourth graph G4.
The magnitude of the reflectance variation (ΔR(Hn+1′″)) at the n+1th highest point of the fourth graph G4 and the sum (i.e., Σi=0i=kΔR(Hn+1+i′″)) of values, from the magnitude of the reflectance variation at the n+1th highest point of the fourth graph G4 to the magnitude of the reflectance variation at an n+k+1th highest point of the fourth graph G4 may have correlation with the thickness of the underlying layer. Thus, if the correlation between these values and the thickness of the underlying layer is obtained from experiment, the thickness of the underlying layer may be measured by measuring these values. For example, the greater the thickness of the underlying layer is, the greater these values may be. There may be a linear relationship between the thickness of the underlying layer and these values.
Referring to
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The thicknesses of the underlying layers of the reference samples were measured using X-ray fluorescence (XRF). The thicknesses of the underlying layers of the reference samples were measured by the method 1000 according to some example embodiments shown in
It was confirmed that the thicknesses of the underlying layers measured by XRF were in a linear relationship with the thicknesses of the underlying layers measured by the method 1000 (refer to
While the present inventive concepts have been particularly shown and described with reference to example embodiments thereof, it will be understood by those of ordinary skill in the art that various changes in form and details may be made therein without departing from the spirit and scope of the present disclosure as defined by the following claims.
Number | Date | Country | Kind |
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10-2018-0171137 | Dec 2018 | KR | national |