Surface Topography of Cuneiform Tablets
Monica Barbu


Introduction

        History is essential to human existence, not only because it holds a record of out past but it also teaches us about the present and can offer a window into the future. Ancient Cuneiform tablets consist of one of the oldest forms of writings in the world.  These clay tablets act as a link between our time and a time thousands of years ago.  The term Cuneiform, which originates from the Latin word cuneus  meaning wedge shaped, evolved from early pictographs.(1) These tablets originate from the lower valley of the Tigris and Euphrates River in Mesopotamia, what is known today as Iraq. The Cuneiform text is considered one of the first forms of writing. The structure of this text did not match the syntax of a spoken language. They were restricted to dealing in lists and categories, as opposed to sentences and narratives used in spoken language today. Most of the Cuneiform tablets were documents about property, inventory and taxes.(2) Along with the wedge shaped marks, these five thousand years old documents bear a feature called cylinder seal impression.  The seal impressions consist of different design elements, which serve to identify their owner or distinguish a specific deity.
        Reconstruction of ancient documents such as the Cuneiform tablets and stilus tablets provide scientists and scholars with the challenge of transforming their three dimensional characteristics to a two dimensional plane. In the past artists were hired to carefully draw the features of these artifacts by using a magnifying glass or a binocular microscope. This was not only time consuming, but arguably, very subjective. Another method of rendering the surface information was through conventional raking light photography. However, because the surface of the Cuneiform tablet subsists of uneven curves and features of various degrees of depth they present many problems to photographers as well as epistolary scholars who try to read and represent these images.
        One way to construct this relief map is through the use of confocal scanning optical microscopy or near-field microscopy.  Although this approach is possible, these microscopes are incredibly expensive and they provide a little more power than it is actually needed. (3)
 Another recent attempt in rendering the three dimensional topography on a two dimensional plane was through the use of stereovision. (4)  Although the idea seems promising, since it has been used in astronomical imagery, it does not seem to be applicable in the cases analogous to that of the Cuneiform tablet.  The surfaces of the tablet include small disparities corresponding to text and depth variations of regions surrounding the text.  These differences and subtle variations require extreme care in choosing correct lenses, baseline separation between the two cameras, as well as the appropriate camera mounting apparatus.  It is evident, that calculating the topography of the Cuneiform tablets from digital images is a great deal more simple and more affordable.
        Calculating the topography of the Cuneiform tablets from digital images is a distinct way to extract contour measurements of the wedge shaped characters and cylinder seal impressions found in their surfaces. Using surface topography techniques previously applied to intaglio prints and lithic artifacts as well as implementation of modern digital image processing techniques, images of the Cuneiform text are displayed in their highest potential of detail and clarity. These techniques not only provide a qualitative result of the surface topography, but more importantly, they present a quantitative analysis of the surface of the tablet.
 
 

Theory

Surface Topography:         The following concepts in regards to surface topography are based on previous work completed by J. S. Arney and D. Stewart.(5) Topography is described as a variation in height, h (x), across a horizontal dimension, x. In order to relate the characteristics of the surface of an object to the variations in irradaince, I (x), detected across the film plane of the camera, it is crucial to have an optical model that relates the two. In this case the irradiance, I (x) = *[h (x)]. In this optical model two assumptions are made. First assumption is that the surface of the object is a Lambertian reflector, which means that the irradiance at the film plane will be independent of the angle of viewing and will depend only on the angle between the surface and the source of illumination. The second assumption is that the object surface is a diffuse reflector.
 
Figure 1. Image capture of surface topography.
 
As a result the light reaching the detector as illustrated in Fig. 1 is controlled by Io, the irradiance of the light incident on the surface of the object, the reflectance factor of the object, R, and the angle of illumination. As a result of these assumptions, one can generate Eq. 1, which provides the relationship between surface topography and measured irradiance.
       (Eq. 1)
Topography can be described in point by point variation in the angle, a(x), between the object and the mean surface of the object. The height variation at a certain location is related to the surface angle through the derivative.
 
 
        (Eq. 2)

 
 

 
Figure 2. Illustrates the relationship between a horizontal slice of an object and the variation in angle, a (x).
 
Furthermore, because of the Lambertian assumption, the variation in the angle, a acts as a variation only in the illumination angle q . Therefore, topographic information can be related to the irradiance of the camera as follows:
  The angle q(x) in the equation above is the sum of the angle of illumination,qo, and the mean surface angle, a (x). As a result from the analysis above a quantitative relationship between the observed irradiance, I(x) and the topography of an object, h(x) can be derived.

The term R(x) in Eq. 3 can be separated from the topographic information, sin[q (x)], by taking the ration of two images captured at two different angle of illumination. The characteristics of the two images in one dimension would be the following:

 

    (Eq. 4)
 
    (Eq. 5)

 

In Eq. 4 and Eq. 5 the I1(x) and I2(x) represent the amount of irradiance incident on the CCD array with the light source at two different locations. Io is the irradiance of the light source. R(x) is the reflectance factor at a certain location. q 01 and q 02 are the angles of illumination. a(x) contains the topographical information.

As a result of taking the ratio between Eq. 4 and Eq. 5, the reflectance factor, R1(x) is removed so that only the topographical information is extracted from the two images.
 

     (Eq. 6)
  Solving Eq. 6 for the topographic features in terms of tan[a (x)} by using appropriate trigonometric identities the following expression is derived.

 

      (Eq. 7)

 

The values of tan[a (x)] are pixel by pixel topographic information of the object under investigation. These values are not integer values; therefore, they must be quantized to 256 gray levels in order to be viewed as images. Taking Eq. 7 along with Eq. 2 the topographic height function can be obtained.
 

    (Eq. 8)

 

Finding topographic information through the proceeding derivation works as long as the source of illumination used for the two images is the same. A novel device was build to help solve this problem. Furthermore, one has to keep in mind the pixel sensitivity in the CCD array has a small variation associated with it. As a result, each image used in the experiment was corrected for this inconsistency by using flat fielding. Flat fielding removes the variation in brightness, which can be caused by the non-uniform illumination and small "dark currents" in the array.

 

 

 

 

 

Methods

Results and Discussion:

Conclusion
 
Table of Contents