We present a study of the Lyman alpha forest of the QSO 1331 + 170 in
the range 1.67 <z(abs) < 2.10 at 18 km s(-1) resolution. Our analysis
includes a careful search for previously unidentified heavy-element sy
stems, and incorporates detailed deblending of Ly alpha forest lines f
rom heavy-element lines. Various statistical properties of Ly alpha fo
rest lines, such as distributions of equivalent widths, HI I column de
nsities, Doppler parameters and pair-velocity separations, are compute
d. The effect on these properties of employing different limiting appr
oaches to heavy-element deblending, and profile-fitting of the lines,
is illustrated. Our data suggest that the N-HI distribution may not be
fitted adequately by a single power law, i.e., that there may be a re
lative deficit of strong lines as compared with the predictions of a s
ingle power law. However, larger samples are required to verify this d
eficit. The median b value is approximate to 32 km s(-1). No significa
nt correlation is observed between N-HI and b. An excess on the scale
of similar to 100 km s(-1) is seen in the pair-velocity correlations,
at the level of similar to 2.6 sigma for the conservative sample and a
t the level of similar to 4.9 sigma for the less conservative sample.
Marginal excess correlation is seen in both the samples at the greater
than or similar to 2 sigma level on scales of similar to 800-1000 km
s(-1), and also on scales of similar to 6000 km s(-1).