Comparison to Other Systems
(Advanced Piston Core and Calypso Core)
By comparing the sediments recovered by KNR191 with
previously recovered core sections, we can evaluate the performance of the new
long coring system. The cea trials
cruise conducted its coring operations at Bermuda Rise at the original site of
KNR31-3-5GPC (33.69º N 57.58º W) . This
location was subsequently cored by the Marion Dufresne Calypso core in 1995 and
by Ocean Drilling Program Leg 172 in 1997.ODP Site 1063 cored the same location four times using the Advanced Piston
Core (APC) system. By its very nature,
the APC provides the ideal standard section to compare with other piston core
systems because the piston is in a fixed position at the bottom of the drill
string and cannot more with respect to the sediments (except for heave related
to sea state conditions, which is common to all coring systems).
Figure 1. GRAPE density records obtained using a Geotek multi-sensor track during KNR191.
Figure 2. GRAPE density records from ODP Site 1063.
Figure 3. The stratigrpahic levels of various features in ODP Site 1063. In this figure ODP 1063A is used as a referencd section and holes 1063B, 1063C, and 1063D are comapred to it. The variability around the 1:1 line is caused by local variability in sedimentation.
Figure 4. The stratigraphic levels of various features in KNR191 long piston cores, referenced to the same level in ODP1063A. KNR191 (red symbols) and ODP1063 (black symbols). For the upper 28 meters of the section, recovery is the same for the new long core system and for the ODP Advanced Piston Core. Below 28 meters the recover is less in three long cores, most likely caused by compression during the late stages of core penetration. For two long cores, we used a reduced diameter core cutter which improved recovery and eliminated sediment compression.
Figure 5. The stratigraphic levels of various features in MD95-2034, referenced to the same level in ODP1063A. MD95-2035 (blue symbols) KNR191 (red symbols) and ODP1063 (black symbols). Slopes higher than 1:1 and lower than 1:1 show intervals in MD95-2034 where stretching and compression (respectively) disturbed the sediment recovery.
We will compare GRAPE density records which were routinely
collected at sea by the KNR191, ODP172, and MD95. These measurements provide easy identifiable
lithostratigraphic measurements to correlate the sections. We arbitrarily choose ODP Hole 1063A as the
standard and compare the sections by identifying equivalent stratigraphic
levels and plotting them in an X-Y plot. .
The first comparison (Figure 3)
compares ODP Hole 1063A with ODP Holes 1063B, 1063C and 1063D. By comparing these four holes, the degree of
local stratigraphic variability can be quantified since these holes were
recovered within tens of meters of one another using the same coring
system. Equivalent stratigraphic levels
fall within 1 meter of each other.
The same comparison including KNR191 piston cores (Figure 4) shows that the new long core system is duplicating the
recovery of the APC for the upper 28 meters or so. Thus there is no evidence of stretching as a
result of the coring process. Below this
level, the recovery for three of the KNR191 cores falls below the recovery for
ODP Hole 1063A, implying that new coring system is compressing the
stratigraphic section during the latest stages of the coring process. For two of the new long cores, this
compression did not occur because we used a core cutter with a diameter just slightly
smaller than the inside diameter of the core liner. We believe that this reduced the internal
friction in the core barrel and enhanced core recovery.
The same comparison using the density record for MD95-2034
(Figure 5) documents that this core suffered from some
stretching in the upper sections and also compression in the lower
sections. (The stretching of this coring
system was first pointed out by Skinner and McCave (2003) by comparing piston
and gravity coring systems at the same location near the Iberian
Last updated: December 20, 2010