Revealing the impact
of core mineral composition on the initiation
pressure of waterflood-induced fractures (WIFs) in tight sandstone
reservoirs is a crucial aspect of studying the initiation mechanism
of WIFs. In this paper, through quantitative characterization of the
core mineral composition from six samples of the Chang 6 reservoir
in the Wuqi oilfield, western Ordos Basin, and modified experimental
cores and displacement equipment for WIF experiments, the influence
of the core mineral composition on the initiation pressure of WIFs
in tight oil reservoirs is investigated. The conclusions are as follows.
(1) The rock mineral composition of the Chang 6 reservoir in the Wuqi
oilfield, western Ordos Basin, includes quartz, feldspar calcite,
and clay, characterizing it as a typical feldspar sandstone reservoir.
Quartz and calcite are considered as brittle minerals, while feldspar
and clay are categorized as lithologic minerals. (2) For feldspar
sandstone reservoirs, including quartz, feldspar, calcite, and clay
minerals, when the combined content of quartz and feldspar exceeds
600% of the total mineral content, the changes of quartz and feldspar
content will affect the initiation pressure of WIFs. As the ratio
of the quartz content to feldspar content R
qf increases, the initiation pressure of WIFs exhibits a logarithmic
function decrease. (3) Considering the contribution of diagenetic
minerals to rock brittleness, the calculation method for the brittleness
index of feldspar tight sandstone reservoirs is improved. (4) The
relationships between R
qf, brittleness
index, and initiation pressure of induced fractures suggest that an
increase in R
qf leads to a power-law increase
in the brittleness index, while the initiation pressure of WIFs relative
to the brittleness index shows a power-law decrease. This phenomenon
indicates an increased likelihood of WIFs occurring during the long-term
water injection process in feldspar sandstone reservoirs. This work
contributes to understanding how core minerals affect the initiation
pressure of WIFs in tight sandstone reservoirs.