Iron-deficiency Clinical Trial
Official title:
Effects of Iron Status, Manipulated Using Intravenous Iron, on Cardiopulmonary Physiology During Ascent to Very High Altitude
This study involved human volunteers undertaking a high-altitude expedition. It assessed changes in physiological parameters of relevance to high-altitude cardiopulmonary physiology. Participants included a subgroup of those taking part in an existing adventurous training expedition and were randomised in a 1:1 fashion to receive either intravenous iron or normal saline several weeks prior to departure. During the expedition, participants were investigated by means of transthoracic echocardiography, peripheral oxygen saturation measurement and heart rate monitoring and through the drawing of venous blood samples. Bloods were later analysed for markers of iron status.
Aim
The aim of the study was to investigate the effects of iron status on human cardiopulmonary
physiology during ascent to very high altitude. Differences in iron status were brought about
using intravenous iron, and outcomes were assessed using echocardiography and self-reported
functional performance scores.
Objectives
Principal objective: To compare echocardiographic parameters in individuals of differing iron
status during the expedition.
Secondary objectives: To compare physiological variables (oxygen saturation, pulse) and
self-reported functional measures, in individuals of differing iron status during the
expedition.
Hypotheses
The primary hypothesis was that iron status, manipulated using intravenous iron, would
influence the echocardiographic indices of cardiopulmonary physiological function over the
course of the ascent.
A secondary hypothesis was that iron status would influence cardiopulmonary responses in
terms of pulse and oxygen saturation, and additionally the perceived exertion involved in
ascent to very high altitude.
Design of the Study
The study randomised 18 individuals to iron or normal saline in a 1:1 ratio giving two groups
of 9 people. The randomised infusion (control or iron) was undertaken at a pre-expedition
meeting approximately 2 weeks prior to the flight to Nepal. The profile of ascent to high
altitude will followed internationally accepted acclimatisation guidelines.
Preliminary Testing
To exclude elevated iron stores prior to enrollment, participants underwent an initial blood
test. At the pre-exercise mounting station, prior to the flight to Nepal, baseline
echocardiography was performed, and blood samples were collected immediately prior to
randomisation and infusion. All blood samples in the study were analysed for full blood
count, ferritin, iron, transferrin and C-reactive protein (CRP).
Expedition-based tests
Waking peripheral oxygen saturation (%) of haemoglobin (SpO2) and pulse were recorded daily.
Venous blood samples were taken for later analysis of variables relevant to iron homeostasis
including full blood count, erythropoietin, soluble transferrin receptor and hepcidin. These
samples were taken in Kathmandu on the morning following arrival, at the intermediate staging
camp (~3,200m) and then at the Dhaulagiri base camp on arrival and after descents from 6,000m
and 7,000m.
Measures of both left and right heart function were performed and included: pulmonary artery
systolic pressure, pulmonary acceleration time, pulmonary regurgitation end diastolic
velocity and tricuspid annular plane systolic excursion (distance of systolic excursion of
the right ventricular annular plane towards the apex - TAPSE). Echo parameters were acquired
and processed by an appropriately experienced researcher. Measures were taken during exercise
on arrival at each test altitude and at rest the following morning. Measurements taken from
climbers returning from either 6,000 m or 7,000 m were taken as soon as possible after their
return to base camp.
Subjective ratings scales include those for breathlessness (Borg 1-10) and perceived exertion
(Borg 6-20).
Blood sample storage and analysis
Once drawn, venous blood was placed on ice. Following centrifugation (3,500 rpm for 10
minutes at 4OC), aliquots of plasma were stored in cryogenic vials at -20°C. Samples drawn at
high altitude were transported on dry ice or in liquid nitrogen 'dry-shippers' (safe liquid
nitrogen containers that cannot leak nitrogen as liquid) back to the UK (United Kingdom).
Subsequent analysis was performed at the University of Oxford.
Statistical analysis
Data were analysed using statistical tests with International Business Machines (IBM)
'statistical package for social sciences' (SPSS) version 22 software.
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