Semiconductor wafer with crystal lattice defects, and...

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Reexamination Certificate

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C428S446000, C117S928000

Reexamination Certificate

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06579589

ABSTRACT:

BACKGROUND OF THE INVENTION
1. Field of the Invention
The present invention relates to a semiconductor wafer with an uneven distribution of crystal lattice defects, and to a process for producing this wafer.
2. The Prior Art
Silicon crystals, in particular for the production of semiconductor wafers, are preferably obtained by pulling a seed crystal from a silicon melt, which is generally provided inside a quartz glass crucible. This so-called Czochralski crucible-pulling process is described in detail in, for example, W. Zulehner and D. Huber,
Czochralski
-
Grown Silicon, Crystals
8, Springer Verlag Berlin-Heidelberg 1982.
Due to the reaction of the quartz glass crucible with the molten silicon during the crucible-pulling process, oxygen is included as the dominant impurity in the growing silicon crystal. The concentration of oxygen is usually so high that, after the crystal has cooled, it is in supersaturated form. In subsequent heat treatments, the oxygen is deposited in the form of oxygen precipitates. These precipitates have both advantages and disadvantages. The so-called gettering properties of the oxygen precipitates are an advantage.
This is understood to mean that, for example, metallic impurities in the semiconductor wafer are bonded to the oxygen precipitates. Thus, they are removed from the layer which is close to the surface and is relevant for components. A drawback is that oxygen precipitates in the layer which is close to the surface. This is relevant for components and will interfere with the function of the components which are manufactured on the semiconductor wafer. Consequently, it is desired for a precipitate-free zone, PFZ, also known as a denuded zone, DZ, to be formed in the vicinity of the surface. It is also desired for a high concentration of precipitates to be formed in the interior of the semiconductor wafer, known as the bulk.
The prior art, for example in “
Oxygen in Silicon”
F. Shimura,
Semiconductors and Semimaterials
Vol. 42, Academic Press, San Diego, 1994, has disclosed how the outdiffusion of the oxygen near the surface is achieved in a heat treatment at temperatures of preferably over 1100° C. As a result of this outdiffusion, the concentration of oxygen in the layer close to the surface falls so far that there is no longer any precipitation, and consequently a PFZ is generated. This heat treatment was in most cases directly integrated into the processes for producing components. In modern processes, however, these high temperatures are no longer used, and consequently the required outdiffusion is brought about by an additional heat-treatment step.
The oxygen precipitation, in particular in crucible-pulled semiconductor material, takes place substantially in two steps:
1) formation of nucleation centers for oxygen precipitates, so-called nuclei;
2) growth of these centers to form detectable oxygen precipitates.
During subsequent heat treatments, the size of these nuclei can be modified in such a way that those which have a larger radius than the so-called “critical radius” grow into oxygen precipitates. On the other hand, nuclei with a smaller radius break down (are dissolved). The growth of nuclei with a radius >r
c
takes place at elevated temperature and is substantially limited by the diffusion of oxygen. A generally accepted model (cf., for example, Vanhellemont et al.,
J. Appl. Phys.
62, p. 3960, 1987) describes the critical radius r
c
as a function of the temperature, the oxygen supersaturation and the concentration of vacancies. Concentration is understood to mean particles per unit volume.
A high oxygen concentration and/or a high vacancy supersaturation simplifies or accelerates the precipitation of oxygen and leads to a higher concentration of precipitates. Furthermore, the concentration or size of the precipitates, in particular in semiconductor wafers, depends on heating and cooling rates during thermal furnace processes, in particular during the so-called RTA (rapid thermal annealing) processes. During these heat treatments, semiconductor wafers are heated to temperatures of up to 1300° C. within a few seconds and are then cooled at rates of up to 300° C./sec.
The oxygen concentration, the vacancy concentration, the interstitial concentration, the dopant concentration and the concentration of existing precipitation nuclei, such as for example carbon atoms, also influence the precipitation of oxygen.
WO 98/38675 has disclosed a semiconductor wafer with an uneven distribution of crystal lattice vacancies, which is obtained by means of a heat treatment. The maximum level of this vacancy profile generated in this way is situated in the bulk of the semiconductor wafer, and the profile decreases considerably toward the surfaces. During subsequent heat-treatment processes, in particular at 800° C. for 3 h and 1000° C. for 16 h, the oxygen precipitation follows this profile. The result is a PFZ without prior outdiffusion of the oxygen and oxygen precipitates in the bulk of the semiconductor wafer.
According to WO 98/38675, the concentration of oxygen precipitates is set by means of the concentration of vacancies, and the depth of the precipitates is set by means of the cooling rate following the heat treatment. A drawback of this semiconductor wafer is that the getter centers are limited to the bulk. Furthermore, very high BMD (bulk micro defect) concentrations lead to high leakage currents from integrated circuits when these circuits are located close to the layer relevant for the components. These leakage currents can be minimized if regions with very high BMD concentrations are produced as far away from the components as possible. Furthermore, it has been found that, in particular for applications in micromechanics, high BMD concentrations in the middle of the semiconductor wafer have an adverse effect on the selective etching behavior. This is because a high variation in etching removal rates is observed in the presence of the precipitates. Consequently, it is desired to limit the oxygen precipitates as far as possible to defined layers. It is also desired to keep the back-side part of the semiconductor wafer precipitate-free, for example for the production of micromechanical structures.
SUMMARY OF THE INVENTION
It is therefore an object of the present invention to provide a semiconductor wafer, and a process for producing the wafer, which serves as a basis for a semiconductor wafer with an improved internal gettering action.
This above object is achieved according to the invention by means of a semiconductor wafer having a front side
1
, a back side
2
, a top layer
3
, a bottom layer
4
, an upper inner layer
5
lying below the top layer
3
, a lower inner layer
6
lying above the bottom layer
4
, a central region
7
between the layers
5
and
6
and an uneven distribution of crystal lattice defects. The concentration of the defects exhibits a first maximum (max
1
) in the central region
7
and a second maximum (max
2
) in the bottom layer
4
.
The defects are preferably vacancies which are converted into nucleation centers for oxygen precipitates during subsequent heat treatment processes, preferably at temperatures of from 300° C. to 800° C. According to the invention, the nucleation centers follow the profile of the vacancies. Preferably, the concentration of the defects increases from the front side
1
of the semiconductor wafer toward the central region
7
, up to the first maximum (max
1
), and toward the bottom layer
4
, up to the second maximum (max
2
).
Accordingly, the above object is also achieved by means of a semiconductor wafer with an uneven distribution of nucleation centers for oxygen precipitates.
In particular, the object is also achieved by means of a semiconductor wafer having a front side
1
, a back side
2
, a top layer
3
, a bottom layer
4
, an upper inner layer
5
lying below the top layer
3
, a lower inner layer
6
lying above the bottom layer
4
, a central region
7
between the layers
5
and
6
and an uneven distribution of nucleation centers for oxygen precipitates. T

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