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TIBIAL SLOPE AND ACL RUPTURE: MRI ASSESSMENT

167

Under normal loading conditions, patients with a

greater lateral PTS may have greater internal

rotations of the lower leg. The resulting internal

rotation stresses the ACL and may increase the

injury risk [15]. Inconsistency was reported by

Hashemi

et al.

[20] in which the male’s medial

PTSwas associatedwith injurybut not the females.

They also observed an increased medial tibial

plateau depth in conjunction with an increased

PTS in patients with noncontact ACL injuries.

The anterior tibial translation increased

significantly after an ACL rupture [25, 26]. It

suggested that the ACL served as the main knee

stabilizer in tibiofemoral translation, with

specific tension being produced in the course of

internal rotation [15]. When an anterior force is

applied to the tibia of the knee with intact

ligaments, the internal rotation that occurs

imparts considerable stress on the ACL [26].

Tibial slope on lateral tibial plateau undertakes

an important role during extension motion

because it favors internal rotation, which, in

turn, imparts considerable stress on the

extended ACL [25].

The PTS plays an important role in knee

replacement, after total knee arthroplasty

(TKA); the posterior tibial slope affects

anteroposterior stability, range of motion, and

contact pressure within the tibiofemoral joint

[28]. Moreover, an inappropriate cutting angle

of the posterior tibial slope results in

polyethylene wear, component loosening and

posterior cruciate ligament strain [29].

During early weight bearing after ACL

reconstruction, a steep tibial slope might place

increased load on the healing graft and fixation

material and potentially increase the risk of

early elongation or acute failure. Improved

knowledge about the effect of the tibial slope

on the graft after ACL reconstruction might

serve as a basis for individually adapted

postoperative rehabilitation programmes [15].

A small increase in tibial slope, which may

occur inadvertently during medial opening-

wedge HTOs, would not adversely affect

overall A-P knee stability or the in situ forces in

the cruciate ligaments. However, the changes

observed in the resting position with

osteotomies in the sagittal plane may be

important in the treatment of cruciate ligament-

deficient knees [30].

Inconsistencies within and between tibial slope

measurement methodologies have precluded

repeatable demonstration of an “at ACL injury

risk” range of tibial slope values.

Identification of new risk factors is paramount to

prevention. While trends in the current literature

indicate a potential relationship between ACL

injury and PTS, standardized techniques and

more consistent and repeatable data are required

to definitively link the two [25].

The future goal of the research relating tibial

plateau slope to ACL injury risk should be to

establish not only the extent of the role of tibial

slope in injury risk but also the extent to which

that risk can be decreased by prophylactic

interventions such as neuromuscular training.

Such methodologies will also enhance the

objectivity of tibial slope as a factor in the

assessment of post-injury stability and long-

term sequelae [25].

Subjects with an increased tibial slope who are

participating in high-risk activities should

perhaps consider prophylactic precautions.

This could include education on the increased

risk for ACL rupture, as well as injury

prevention training [5].

One of the limitations of the present study is

that we did not have access to the height and

weight of the subjects, and consequently we

did not explore correlations that may exist with

the measured slopes. These parameters should

be tested in future. Secondly, it is important to

note that the MRI voxel resolution, the access

to a sufficient length of the tibia and the ability

to identify landmarks precisely all could have

an impact on the slope measurements.

However, although these factors may influence

the results, they will not influence the large

inter individual differences or the large range

of slope values.