2007, Piran, Slovenia

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Environmental Ergonomics XII Igor B. Mekjavic, Stelios N. Kounalakis & Nigel A.S. Taylor (Eds.), © BIOMED, Ljubljana <strong>2007</strong> DISCUSSION Therefore, it was concluded that the present mathematical model of sweat rate was suited not only for younger males, but also for younger females and the elderly. ACKNOWLEDGEMENTS This research was supported in part by a Grant-in-Aid for Scientific Research (No.16207017) by the Japanese Society for the Promotion of Science. REFERENCES Yokoyama, S., 1993. Heat Transfer Phenomena within Human Body. Hokkaido University Press, Sapporo. Yokoyama, S., Kakuta, N., Ochifuji, K., 1997. Development of a New Algorithm for Heat Transfer Equation in the Human Body and its Applications. Appl. Human Sci., 16, 153- 159. Yokoyama, S., Kakuta, N., Togashi, T. Hamada, Y., Nakamura., MA., Ochifuji, K., 2000a, Development of Prediction Computer Program of Whole Body Temperature Expressing Local Characteristics of Each Segment : Part 1 Bio-Heat Equations and Solving Method. Trans SHASE, 77, 1-12. Yokoyama, S,, Kakuta, N., Togashi, T., Hamada, Y., Nakamura, MA., Ochifuji, K., 2000b, Development of Prediction Computer Program of Whole Body Temperature Expressing Local Characteristics of Each Segment : Part 2 Analysis of the Mathematical Model for the Control of Skin Blood Flow. Trans SHASE, 78, 1-8. Yokoyama, S., Kakuta, N., Togashi, T., Nakamura, MI., Masaki, T., Hamada, Y., Nakamura, MA., Ochifuji, K. 2002, Development of Prediction Computer Program of Whole Body Temperature Expressing Local Characteristics of Each Segment : Part 3 Comparison of Measured and Calculated Results. Trans SHASE, 84, 43-52. Yokoyama, S., Tao, M., Kakuta, N., <strong>2007</strong>, Prediction Computer Program of Whole Body Temperatures and its Application under the Various Combinations of Working Level and Thermal Environmental Condition. Industrial Health, 45, 118-124. 282
Sweating REGIONAL FOOT SWEAT RATES DURING A 65-MINUTE UPHILL WALK WITH A BACKPACK Alison L. Fogarty 1 , Rebecca Barlett 1 , Vincent Ventenat 2 , George Havenith 1 1 Loughborough University, United Kingdom, 2 Centre de Recherche DECATHLON, Villeneuve d'Asq - France. Contact person: G.Havenith@lboro.ac.uk INTRODUCTION As recently demonstrated by Taylor et al. (2006), all regions of the foot participate in thermoregulatory sweating when under sufficient thermal and exercise loading. Their measurements were taken using capsules during one-legged cycling with the measurements taken on the passive foot only, assuming equal sweat rates in the passive foot to the contralateral active foot. The reason for using the passive foot is the problem that the capsules cannot easily be used inside footwear, and that the capsule connection tubing is difficult to keep in place on moving feet. The current study therefore made an attempt to investigate local sweat rates of an active foot while walking uphill for 65 minutes. Furthermore, during the present study walking boots and socks were worn. To our knowledge, no other study has measured sweat rates on an exercising foot. METHODS Nine regularly active males completed a 65-min uphill treadmill walk (5 km.hr -1 , 10% grade) carrying a 15-kg backpack with ambient conditions of 25.9 ±0.6ºC and 48.6% relative humidity. Sweat rates were measured using an absorption method developed in our laboratory. Briefly, proportional patches of a non-woven absorbent material were applied to pre-determined zones for 10 minutes on the right foot. The foot was divided into 6 zones: 3 plantar regions (toes, mid-sole and heel), and three dorsal regions (medial, central and lateral). A 5 x 2.5cm patch was also taped to the forehead. Sweat rates were calculated from the change in mass of the patches before and after application and expressed in g.m -2 .hr -1 . Sweat rate was measured for 10 min, 3 times during the trial: at 0 min, 30 min and 50 min. Local foot temperatures were estimated from infra-red thermal images of the towel-dried skin taken at baseline and after each sweat sampling period. Cardiac frequency (fc) was measured every 15 sec, whereas auditory canal temperature (Tau) was measured at the start and end of the trial. RESULTS Cardiac frequency averaged 127.13 beats.min -1 and Tau increased by an average of 0.5ºC. The local foot temperatures were uniform across the zones, starting at 29.4ºC and stabilising at 34.9ºC by the end of the trial. Foot sweat rates increased from 212 to 416 and 366 g.m -2 .h -1 and forehead ranged from 150 to 598 and 638 g.m -2 .h -1 across the 3 sample periods. Forehead sweating was lower than all foot samples at the first sample but had the highest sweat rate for the 2 nd and 3 rd samples. For the 2 nd and 3 rd samples, the sweating pattern was similar with all plantar regions producing less sweat than the dorsal regions (33% and 66% of total foot sweat respectively). These percentages concur with Taylor et al. (2006) who reported 30% and 70% of foot sweat being produced on the plantar and dorsal regions respectively. There was a tendency for sweating to be slightly reduced towards the end of the walking period, especially on the dorsal regions, which may indicate hidromeiosis. 283
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ENVIRONMENTAL ERGONOMICS XII Procee
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ENVIRONMENTAL ERGONOMICS XII Procee
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International Conferences on Enviro
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TABLE OF CONTENTS Table of contents
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Table of contents ALTITUDE ATTENUAT
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Table of contents TOWARDS PREVENTIO
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Table of contents RATE AFFECT EXERC
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Table of contents Uroš Dobnikar, S
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Table of contents TO A HOT ENVIRONM
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Table of contents Andreas D. Flouri
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Table of contents PHYSICAL FITNESS
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Table of contents ESTIMATION OF THE
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Herman Potocnic Lecture the advanta
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Invited presentation Gravitational
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Gravitational Physiology SKELETAL M
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Lf (mm) 50.0 40.0 30.0 20.0 10.0 Fa
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Gravitational Physiology maximum is
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Gravitational Physiology THERMOREGU
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Gravitational Physiology THE EXERCI
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Gravitational Physiology Since exer
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Gravitational Physiology During the
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Gravitational Physiology CARDIOVASC
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as observed at rest after LBNP was
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Gravitational Physiology THERMOREGU
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Gravitational Physiology THE EFFECT
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Gravitational Physiology Fortney SM
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Gravitational Physiology Contractil
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Gravitational Physiology Edgerton V
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Diving Physiology A library of imag
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Diving Physiology Information recal
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Diving Physiology RESULTS Figure 1
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Diving Physiology sensitivity is no
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Diving Physiology Physiological Mea
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Diving Physiology same sequence. Th
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Diving Physiology HYPERVENTILATION
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Diving Physiology software. Individ
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Diving Physiology REFERENCES IMCA.
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Diving Physiology recorded (MIE Med
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Diving Physiology DISCUSSION The ma
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Altitude Physiology vastus laterali
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Altitude Physiology IS INTERMITTENT
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Altitude Physiology Table 2: Lactat
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Altitude Physiology CARBOHYDRATE IN
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Altitude Physiology Figure 1: Mean
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Altitude Physiology HYPOXIA INDUCED
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Altitude Physiology Figure 1. Mean
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Altitude Physiology ANALYSIS OF MUS
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SOL MG TA BF VM Altitude Physiology
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Altitude Physiology LOAD CARRIAGE I
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Table 2: Differential ratings of pe
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Altitude Physiology EFFECTS OF INTE
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Cerebral deoxy-Hb (delta, µM) Cere
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Altitude Physiology ENDURANCE RESPI
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Altitude Physiology Wylegala JA, Pe
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Invited presentation Cognitive and
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Cognitive and Psycophysiological Fu
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Cognitive and psychophysiological f
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CLOTHING AND TEXTILE SCIENCE 131
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Clothing SPACER FABRICS IN OUTDOOR
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F i / g m -2 4,0 3,5 3,0 2,5 2,0 1,
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Clothing TOTAL EVAPORATIVE RESISTAN
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9,0 8,0 7,0 6,0 5,0 4,0 3,0 2,0 1,0
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Clothing DIFFERENCES IN CLOTHING IN
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Clothing parallel It values ranged
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Clothing CORRELATION BETWEEN SUBJEC
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Clothing and left side chest, scapu
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Clothing studies using an ice vest
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Insulation (Clo) (Clo) Clo / kg 6 5
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Clothing EFFECTS OF MOISTURE TRANSP
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Clothing the P plots above 60%RH (p
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Clothing EFFECT OF CLOTHING INSULAT
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Clothing EFFECTS OF QUILT AND MATTR
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38 33 28 23 18 0 30 60 90 120 150 m
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Clothing German) were measured, and
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Clothing Metabolism decreased and w
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Clothing Table 1. Comparison of ski
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Clothing PHYSIOLOGICAL RESPONSES AT
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Clothing underwear at 25 °C in per
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Clothing REDUCTION OF HEAT STRESS I
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Clothing THE INTERACTION BETWEEN PH
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Relative humidity (%) Clothing Figu
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Clothing DEVELOPMENT OF THE “WEAR
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Clothing EFFECTS OF AIR GAPS UNDER
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Temper at ur e( ˇ ć) 28.5 27.5 26
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Personal protective equipment Invit
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Personal protective equipment fabri
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Personal protective equipment PHYSI
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Mean skin temperature (ºC) 38.0 37
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Personal protective equipment the S
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Personal protective equipment DISCU
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Personal protective equipment Final
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Personal protective equipment REFER
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Personal protective equipment Tc wa
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Personal protective equipment level
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F i / g m -2 300 250 200 150 100 50
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h M / % 90 80 70 60 50 40 activity
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Personal protective equipment 0.05
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Personal protective equipment was u
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Personal protective equipment THERM
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Personal protective equipment the s
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Personal protective equipment the c
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Personal protective equipment wette
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Table 1 1. Properties of the tested
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Personal protective equipment HEAT
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Personal protective equipment Profi
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Personal protective equipment PHYSI
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Personal protective equipment REDUC
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Page 241 and 242: Invited presentation Non-thermal fa
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Page 267 and 268: Sweating Table 1: Sweat gland count
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Page 281: Sweating In addition local sweating
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Page 307 and 308: Cold physiology INTRA-INDIVIDUAL DI
Page 309 and 310: Cold physiology number was estimate
Page 311 and 312: Cold physiology cold receptors decr
Page 313 and 314: Cold physiology EFFECT OF URAPIDIL
Page 315 and 316: Cold physiology THE EFFECT OF EXERC
Page 317 and 318: TRAINABILITY OF COLD INDUCED VASODI
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Page 325 and 326: Cold physiology SKIN SURFACE MENTHO
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Cold water immersion the formula: M
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Cold water immersion REFERENCES Cho
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Cold water immersion were: 1 metre
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Cold water immersion surf beaches.
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Cold water immersion Table 1. Break
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Cold water immersion ARM INSULATION
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Cold water immersion RESULTS Experi
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Cold water immersion thermogenesis
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Cold water immersion The other comp
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Cold water immersion REFERENCES And
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Thermal comfort THERMAL SENSATIONS
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Exer - cise PC Wind (m·s -1 ) 0 ne
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Thermal comfort and heart rate usin
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Thermal comfort A NEW METHOD FOR EV
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Thermal comfort DEVELOPMENT OF AN I
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Thermal comfort DISCUSSION This new
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Thermal comfort limit of exposure d
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Table 2: Statistical summary. Gende
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Thermal comfort comfortable”), wh
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Thermal comfort RELATION BETWEEN TH
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Thermal comfort Figure 2. Skin wett
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Thermal comfort THE EVALUATION OF T
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Temp.ˇ ]˘ Jˇ ^ 42 40 38 36 34 32
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time(min) Thermal comfort WHY DO JA
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Thermal comfort TCT : THERMAL COMFO
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Thermal comfort INTERNATIONAL STAND
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Acute and chronic heat exposure PHY
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Acute and chronic heat exposure Fig
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Acute and chronic heat exposure EFF
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Acute and chronic heat exposure 2.2
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Acute and chronic heat exposure EFF
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Acute and chronic heat exposure A N
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Acute and chronic heat exposure of
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Acute and chronic heat exposure PHY
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Acute and chronic heat exposure Tab
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Acute and chronic heat exposure INT
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probability plot 99 95 80 60 40 20
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Acute and chronic heat exposure HAN
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Acute and chronic heat exposure ALL
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Acute and chronic heat exposure Tab
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Acute and chronic heat exposure UNC
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Thermal Sensation Scale 10 9 8 7 6
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Acute and chronic heat exposure RES
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Acute and chronic heat exposure eve
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Acute and chronic heat exposure 30%
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Acute and chronic heat exposure REF
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RADIANT FLOW THROUGH BICYCLE HELMET
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Figure 2. Difference in heat transf
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Manikins DEVELOPMENT OF A LYING DOW
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IT = 6.45( _ ,Tsk - _ ,Tair)/(Q/A)
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Manikins cases. If the body is even
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Heat balance components 100% 80% 60
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Manikins clothing system. This effe
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Manikins The coupled system was val
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Manikins A NOVEL APPROACH TO MODEL-
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Manikins THERMAL MANIKIN EVALUATION
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SR (g/min) Figure 2. Predictive mod
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ESTIMATION OF COOLING EFFECT OF ICE
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Manikins Figure 3: Comparison among
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Manikins EVALUATION OF THE ARMY BOO
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Ty [Nm] 60 50 40 30 20 10 0 0 5 10
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Manikins different black 100% cotto
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Manikins REFERENCES Bogerd, C.P., H
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Modelling RESULTS From this kind of
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Modelling (T , T , V& , ) = 1. 0 +
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NORMALIZED CVCL 8 7 6 5 4 3 2 1 0 M
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Modelling illustrated in Figure 1.
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Modelling MODELLING PATIENT TEMPERA
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Modelling Figure 1: Blood and mean
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Modelling simulations the additiona
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Modelling Table 1. Descriptive summ
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Modelling concomitant increase in b
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Modelling REFERENCES 1. U.S. Depart
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Modelling from the 1988 population.
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Modelling somatotypes in multivaria
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Modelling Each scan data was first
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Modelling The line through the data
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Hip( width) −Waist ( width ) HW
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Modelling measurements are extracte
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Measurement methods not included in
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Measurement methods humidity. The o
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Measurement methods DISCUSSION Base
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Air film Skin surface Skin layer δ
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Measurement methods and calculated
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Rectal temperature ( o C) 39.5 39.0
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Measurement methods work rates, and
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Measurement methods HUMIDEX: CAN TH
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Measurement methods highlighted. In
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Invited presentation Universal Ther
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Universal Thermal Climate Index dat
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Universal Thermal Climate Index DYN
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Universal Thermal Climate Index DIS
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Universal Thermal Climate Index COM
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Skin temperature (°C) Universal Th
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Universal Thermal Climate Index PRO
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Universal Thermal Climate Index The
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Universal Thermal Climate Index ASS
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Universal Thermal Climate Index ima
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Universal Thermal Climate Index min
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Working environment EFFECTS OF LIGH
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Working environment It is interesti
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30 25 20 15 10 5 0 25 12 Working en
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Working environment ERGONOMICS OPTI
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Working environment astigmatism, an
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Working environment RESULTS The hig
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Working environment hearing protect
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Working environment Redistribution
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Working environment DISCUSSION Thes
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Working Environment over the phone
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Working Environment DISCUSSION Diff
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Working Environment results, conclu
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Working Environment BP as the refer
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Working Environment significantly a
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Working Environment responses betwe
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Working Environment Casualty handli
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Working Environment REFERENCES Davi
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Working Environment RESULTS The sub
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Temperature (C) 35 33 31 29 27 25 2
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Working Environment METHODS Student
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Working Environment ANTHROPOGENIC I
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Working Environment RESULTS The res
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Employment Standards VISUAL ACUITY
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Employment Standards Results are pr
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Employment Standards to spend free
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Occupational Thermal Problems and d
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Occupational Thermal Problems HEAT
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Occupational Thermal Problems some
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Occupational Thermal Problems HORSE
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Occupational Thermal Problems range
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Occupational Thermal Problems PHYSI
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Occupational Thermal Problems DISCU
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Occupational Thermal Problems recom
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DLEmin [hours] 7,0 6,0 5,0 4,0 3,0
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Occupational Thermal Problems EFFEC
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Occupational Thermal Problems PERIP
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Occupational Thermal Problems durin
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Occupational Thermal Problems PRODU
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Time (hours) 4 3,5 3 2,5 2 1,5 1 0,
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Occupational Thermal Problems (Suun
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Occupational Thermal Problems highl
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Occupational Thermal Problems and o
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1) estimated (208 - 0.7 x age) *P
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Occupational Thermal Problems of a
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Occupational Thermal Problems tempe
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Table 1: Environmental conditions o
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Occupational Thermal Problems The h
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Occupational Thermal Problems RESUL
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Occupational Thermal Problems PHYSI
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Occupational Thermal Problems corre
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Occupational Thermal Problems DEVEL
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Occupational Thermal Problems All i
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A Adolfsson Niklas 540 Ainslie Phil
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Kim Myung-Ju 409 Kim Taegyou 189 Kl
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Sormunen Erja 599 Spindler Uli 145
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SPONSOR 641
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