“…Articular cartilage can be divided into four zones, namely the superficial zone, the transitional or middle zone, the radial zone and the calcified zone, which have variable structural organization reflected by the variation in T2 ranging from ~20 to 40 ms for superficial layer to sub-millisecond for calcified cartilage [4][5][6][7][8][9]. Most of the currently available clinical and research MR imaging techniques, including proton-density weighted Fast Spin Echo (FSE) [10], T2-weighted FSE [11], gradient echo imaging [12], magnetization transfer [13], T2 mapping [14], delayed Gadolinium enhanced MR imaging (dGEMRIC) [15], and steady State Free Precession (SSFP) imaging [16][17][18] have focused on the superficial layers of cartilage. The study of early and late alterations to the deeper layers of cartilage, including the deepest radial zone and calcified cartilage, has been overlooked due to technical limitations (i.e., the minimal achievable TEs are too long to detect signal from the deeper layers of cartilage because of their very short T2s).…”