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Using the %renal uptake of Tc-99m DTPA and Cr-51 EDTA GFR, a revised equation for GFR was established through linear regression analysis.
We calculated the eGFR using a revised equation for the Japanese population: eGFR (mL/min/1.73 m) = 194 × serum creatinine−1.094 × age−0.287 × 0.739 (if female) [ 11].
GFR measurement using Tc-99m DTPA scintigraphy could be significantly improved by a revised equation derived from the comparison with Cr-51 EDTA GFR.
A revised equation, the Chronic Kidney Disease Epidemiology Collaboration (CKD-EPIcreatinine) produces less biased estimates of GFR at higher levels of kidney function [ 10], although reportedly less accurate estimates as GFR falls below 60 m[/min/1.73 m[ 23].
Renal function was calculated using the estimated glomerular filtration rate (eGFR) with a revised equation for the Japanese population, as follows: eGFR (ml/min/1.73 m) = 194 × (serum creatinine)− 1.094 × (age)− 0.287 × 0.739 (for women) (Matsuo et al., 2009).
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On this view, the revised equation can no longer be claimed to represent a pure unidimensional model.
The revised equation provides consistent predictions of the required length of a grate inlet on a sloping street.
Equation (2) shows the revised equation.
We recommend the use of the LoI method with the improved factor for conversion of OM to C content, or where bulk density is known the Warren equation for calculating accurate C density values across intact and logged forests on Indonesian peats, and our revised equation for oil palm sites.
Using linear regression, the initial equation, the revised equation (including the 5 µg data), and the final equation (including both the 5 µg and 20 week data) yielded R2 values of 0.987, 0.987 (not shown), and 0.990, respectively (Figure 2E).
Next, we retrospectively applied the improved GFR from the revised equation to patients following partial nephrectomy (n = 25).
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