What volume to choose to assess online Kt/V?

Introduction Urea distribution volume (V) can be assessed in different ways, among them the anthropometric Watson Volume (V W ). However, many studies have shown that V W does not coincide with V and that the latter can be more accurately estimated with other methods. The present multicentre study w...

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Published inJournal of nephrology Vol. 33; no. 1; pp. 137 - 146
Main Authors Casino, Francesco Gaetano, Mancini, Elena, Santarsia, Giovanni, Mostacci, Salvatore Domenico, D’Elia, Filomena, Di Carlo, Maria, Iannuzzella, Francesco, Rossi, Luigi, Vernaglione, Luigi, Grimaldi, Daniela, Rapanà, Renato, Basile, Carlo
Format Journal Article
LanguageEnglish
Published Cham Springer International Publishing 01.02.2020
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ISSN1121-8428
1724-6059
1724-6059
DOI10.1007/s40620-019-00636-9

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Summary:Introduction Urea distribution volume (V) can be assessed in different ways, among them the anthropometric Watson Volume (V W ). However, many studies have shown that V W does not coincide with V and that the latter can be more accurately estimated with other methods. The present multicentre study was designed to answer the question: what V to choose to assess online Kt/V? Materials and methods Pre- and postdialysis blood urea nitrogen concentrations and the usual input data set for urea kinetic modelling were obtained for a single dialysis session in 201 Caucasian patients treated in 9 Italian dialysis units. Only dialysis machines measuring ionic dialysance (ID) were utilized. ID reflects very accurately the mean effective dialyser urea clearance (Kd). Six different V values were obtained: the first one was V W ; the second one was computed from the equation established by the HEMO Study to predict the single pool-adjusted modelled V from V W (V H ) (Daugirdas JT et al. KI 64: 1108, 2003); the others were estimated kinetically as: 1. V_ID, in which ID is direct input in the in the double pool variable volume (dpVV) calculation by means of the Solute-solver software; 2. V_Kd, in which the estimated Kd is direct input in the dpVV calculation by means of the Solute-solver software; 3. V_KTV, in which V is calculated by means of the second generation Daugirdas equation; 4. V_SPEEDY, in which ID is direct input in the dpVV calculation by means of the SPEEDY software able to provide results quite similar to those provided by Solute-solver. Results Mean± SD of the main data are reported: measured ID was 190.6 ± 29.6 mL/min, estimated Kd was 211.6 ± 29.0 mL/min. The relationship between paired data was poor (R 2  = 0.34) and their difference at the Bland–Altman plot was large (21 ± 27 mL/min). V W was 35.3 ± 6.3 L, V H 29.5 ± 5.5, V _ ID 28.99 ± 7.6 L, V _ SPEEDY 29.4 ± 7.6 L, V_KTV 29.7 ± 7.0 L. The mean ratio V W /V_ID was 1.22, (i.e. V W overestimated V_ID by about 22%). The mean ratio V H /V_ID was 1.02 (i.e. V H overestimated V_ID by only 2%). The relationship between paired data of V_ID and V W was poor (R 2  = 0.48) and their mean difference at the Bland–Altman plot was very large (−  6.39 ± 5.59 L). The relationship between paired data of V_ID and V H was poor (R 2  = 47) and their mean difference was small but with a large SD (− 0.59 ± 5.53 L). The relationship between paired data of V_ID and V_SPEEDY was excellent (R 2  = 0.993) and their mean difference at the Bland–Altman plot was very small (− 0.54 ± 0.64 L). The relationship between paired data of V_ID and V_KTV was excellent (R 2  = 0.985) and their mean difference at the Bland–Altman plot was small (− 0.85 ± 1.06 L). Conclusions V_ID can be considered the reference method to estimate the modelled V and then the first choice to assess Kt/V. V_SPEEDY is a valuable alternative to V_ID. V_KTV can be utilized in the daily practice, taking also into account its simple way of calculation. V W is not advisable because it leads to underestimation of Kt/V by about 20%.
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ISSN:1121-8428
1724-6059
1724-6059
DOI:10.1007/s40620-019-00636-9