The ion total transports in the near-Earth plasma sheet have been investigated and quantified. Specifically, the net O⁺ transport is about 10²⁴ s⁻¹ in the earthward direction, which is 1 order of magnitude smaller than the typical O⁺ ionospheric outflows, strongly indicating that most outflow will eventually escape, leading to significant atmospheric loss. The study also shows that low-velocity flows (< 100 km s⁻¹) dominate the mass transport in the near-Earth plasma sheet.