K. Kirsch

An overview of experimental investigations into the use of the voice pitch mode (F0 m) as a distance tool for the monitoring of emotional stress reactions is given. Seven experiments are summarized describing the relations between voice reaction and psychological and physical load in laboratory and field applications. The reactivity of F0 m to mental load depends on psychological personality traits. F0 m is less related to physical load. The evaluation of F0 m as voice stress indicator requires an individual calibration. This calibration has to include the assessment of the individual Autonomic Outlet Type (AOT) because the physiological relevance of voice reactions depends on the individual AOT. The calibration is based on statistical reference data which have to be improved in the future. The calibration has to be done under comparable environmental circumstances. A 3-yr application of the method on board Mir station documents the applicability of the procedure.

This report will compare results of applications of the psychophysiological method "Assessment of Autonomic Outlet Type" (AOT) in space as well as at high altitudes. The aim was to find out whether it is possible to differentiate a subject's reaction to different environments by this method (Johannes et.al. 1995). This assessment as described below was first applied to clinically well defined cohorts and to healthy subjects. By means of cluster analysis it could be demonstrated that different reaction patterns exist. These different patterns were correlated to two groups of normal controls ([I] = non-responder/voice-responder and [II] = heart-responder) and two groups of patients with different clinical diagnoses (rheumatic diseases ([III] = autonomic-responder) and [IV] = hypertensives). Based on these clinical reference data the method provides for each "new" experiment a common classification of the complex regulatory reaction pattern of the autonomic nervous system (ANS) and the Cardiovascular system (CVS) to psychological stressors by means of a discriminant function. Since August 1997 the experiment has been applied to all Russian cosmonauts continuously each month. (Johannes et.al. 1998). At the same time numerous terrestrial experiments have been running parallel for comparison with the results from space. This report will focus on a study at altitudes of 3600 m.

Based on data of former clinical studies (Johannes et al. 1994) the experiment regulation was designed to assess and classify the actual psychophysiological reactivity of the cosmonauts. Beside this scientific main goal of the experiment it was for us of interest to check the data whether the development of arrhythmia can be seen under micro-g conditions when flight related stressful conditions prevail. This report will focus on the ECG analysis of one subject in whom this was actually the case.

The aim of this study was to investigate fluidregulating mechanisms, with special regard to the role of plasma proteins in the control of plasma volume (PV), and the role of the superficial tissues as a water storage organ of the body during prolonged physical strain. 29 male subjects (mean age 22.2 +/- 2.8 years) were studied during a 5 day period of survival training with multifactorial strain including restricted water intake (11 H2O.day-1) and food intake (628 kJ.day-1) additionally to physical exercise and sleep deprivation (20 h within 5 days). Under field conditions the heart rate was monitored continuously, and body mass, body composition, thickness of the shell tissues, and blood parameters were measured at (T1), after 72 h (T2), after 120 h (T3) and in the recovery period after 48 h (T4) and 72 h (T5). The estimated energy expenditure was approximately 24,000 kJ.day-1. The mean decrease of body mass was 6.77 kg (9.5%) at T3 (p < 0.001), 0.95 kg (1.3%) at T4 (p < 0.05) and 0.68 kg (0.9%) at T5 (n.s.). A reduction of total body water of 3.8 1 was estimated at T3. Serum creatinine ([Cr]) was raised at T3 by 18.5% (p < 0.0001). No relationship was found between [Cr] and other parameters. The PV decreased by 3.7% (p < 0.0001) at T2, increased by 1.6% (p < 0.0001) at T3 and was not different to baseline at T4 (+0.2%; n.s.). Total protein concentration ([TP]) increased at T2 (11.7%; p < 0.0001) and T3 (2.6%; p < 0.01), and decreased (p < 0.0001) at T4 (8.2%) and T5 (5.7%). Plasma proteins shifted into the intravascular space at T2 and T3 and moved out of the intravascular space at T4 and T5. This gives support to the hypothesis that one of the counterregulatory mechanisms maintaining PV during prolonged exercise is provided by protein shifts from the extravascular into the intravascular space. Our data provide evidence that this mechanism assists PV homeostasis efficiently over a period of 120 h with multifactorial strain, even under conditions with a fluid loss of almost 8% of the total body water.

To quantify fluid distribution at a moderate altitude (2,315 m) 29 male subjects were studied with respect to tissue thickness changes [front (forehead), sternum, tibia], changes of total body water, changes of plasma volume, total protein concentrations (TPC), colloid osmotic pressure (COP), and electrolytes. Tissue thickness at the forehead showed a significant increase from 4.14 mm to 4.41 mm 48 h after ascent to the Rudolfshuette (2,315 m) (P < 0.05). At 96 h after ascent the tissue thickness at the tibia was decreased to 1.33 mm compared to the control value of 1.59 mm (P < 0.01). Body mass increased from 75.5 kg (control) to 76.2 kg on the last day (P < 0.05) and body water from 44.21 to 45.01 during the week (P < 0.01). The accumulation fluid in the upper part of the body was paralleled by a decrease in TPC and COP. At 48 h after the ascent COP dropped from 29.5 mmHg to 27.5 mmHg (P < 0.01). After 96 h at moderate altitude COP was still significantly decreased compared to the control level. At 1.5 h after the return from the Rudolfshuette in Saalfelden (744m) COP was back to the control values. The TPC also showed an initial drop from 7.75 g · dl⁻¹ to 7.48 g · dl⁻¹ after 48 h at altitude and remained below the control value during the whole week (P < 0.01). It seems from our study that even with exposure to moderate altitude measurable fluid shifts to the upper part of the body occurred which were detected by our ultrasound method.

The aim of this study was to determine what effects social isolation and confinement stress had on the volume regulating hormones. In six healthy male subjects, during a 28-d isolation and confinement study (ESA-ISEMSI'90), hematocrit, blood pressure and resting heart rate, plasma cortisol, renin, aldosterone, arginine vasopressin levels besides the electrolyte (Na+, K+) balance and plasma creatinine were measured. During the confinement, an elevated systolic blood pressure (p < 0.01) was observed together with an increase in MHPG corresponding to an elevated mental work load. The pattern displayed by volume regulating hormones (increased values for renin, aldosterone (p < 0.05) and arginine vasopressin) was not only characteristic of confinement stress but also reflected changes in the water and electrolyte metabolism. The increased creatinine levels seen throughout the study were regarded as consequences of hypohydration, and an enhanced muscular catabolism due to reduced physical activity. A similar pattern of hormone modifications was obtained in a head down tilt of the same duration, indicating that some of the described modifications are probably related to isolation and confinement stress.

Intake and output of water were studied in six male subjects from six European countries during 28 days of isolation and confinement in order to assess whether the observed reactions can be compared with those observed during space travel. On the average, the subjects drank 17.5 ml/kg/day fluids. An additional 25 ml/kg/day was recruited from food intake and metabolism. The lowest fluid intake of 11.3 and 12.1 ml/kg/day was shown by two subjects who concurrently lost 3 to 4% of body weight. Three subjects maintained body weight, and one subject gained. A linear correlation existed between the total water output and the fluid intake by drinking. The time series of fluid intake, urine output, and sodium excretion revealed a weekly pattern for these parameters, characterized by low values on Sundays and high values on Fridays. This pattern was most apparent for sodium excretion. Low water turnover rates were seen in the first week of isolation; in the last week the values were above average. In conclusion, it can be said that with respect to the water balance, strong individual differences and time dependent variations (day to day, week to week) of the respective parameters have to be taken into account for the data analysis during such long-term studies.