Helium diffusion in rutile and titanite, and consideration of the origin and implications of diffusional anisotropy

Diffusion of helium has been characterized in natural sphene (titanite) and synthetic rutile. Polished slabs of sphene and rutile were implanted with 100 keV 3He at a dose of 5 × 1015 3He/cm2 and annealed in 1-atm furnaces. 3He distributions following experiments were measured with nuclear reaction analysis using the reaction 3He(d,p)4He. For diffusion in rutile we obtain the following Arrhenius relations: D ‖ a = 2 . 26  ×  1 0 − 1 0 exp ( − 126 ±  11 kJ mol − 1 / RT )  m 2 sec − 1 . D ‖ c = 1 . 75  ×  1 0 − 8 exp ( − 12 0 ±  7 kJ mol − 1 / RT )  m 2 sec − 1 . gh activation energies for diffusion parallel to the c- and a-axes are comparable, there is marked diffusional anisotropy, with diffusion parallel to the c-axis about 2 orders of magnitude faster than transport parallel to the a-axis. These diffusivities bracket the values determined for He diffusion in rutile in bulk release experiments (Stockli et al., 2005, 2007; Wolfe, 2009), although the role of anisotropy could not be directly evaluated in those measurements. anite, the following Arrhenius relation was obtained over the temperature range 252–550 °C for diffusion parallel to the a-axis: D = 2 . 14  ×  1 0 − 6 exp ( − 148 ±  8 kJ mol − 1 / RT )  m 2 sec − 1 . trast to rutile and zircon (Cherniak et al., 2009), titanite shows little evidence of anisotropy, as diffusivities parallel to the a- and c-axes are similar, and diffusivities for titanites from two different localities are similar. He diffusion coefficients obtained in this study are similar to those measured through bulk release of He by step heating (Shuster et al., 2003). Over the investigated temperature range, diffusion of He in titanite is similar to that of He diffusion in rutile parallel to the c-axis, but much faster than diffusion parallel to the a-axis. the diffusion of He in rutile exhibits such pronounced anisotropy, we model diffusional loss of He with a recently developed finite-element code (Watson et al., 2010) created to simulate diffusion in cylindrical geometry with differing radial and axial diffusion coefficients. We present example applications to evaluate helium losses from rutile grains as a function of grain size and length to diameter ratios. orts to better understand the occurrence of pronounced anisotropy for He diffusion in some crystals (e.g., rutile, zircon) but not in others (e.g., apatite, titanite), we consider the density and distribution of interstitial apertures in the crystal structure that might permit He migration. These determinations, an extension of the concept of ionic porosity, are consistent with observations of relative diffusivities and the existence or absence of significant anisotropy for the minerals rutile, zircon, apatite and titanite.