scholarly journals Exposure and Respiratory Tract Deposition Dose of Equivalent Black Carbon in High Altitudes

Atmosphere ◽  
2020 ◽  
Vol 11 (6) ◽  
pp. 598
Author(s):  
Leizel Madueño ◽  
Simonas Kecorius ◽  
Marcos Andrade ◽  
Alfred Wiedensohler
Keyword(s):  
Black Carbon ◽  
Sea Level ◽  
Minute Ventilation ◽  
Personal Exposure ◽  
Total Daily Dose ◽  
High Altitudes ◽  
La Paz ◽  
Pollution Levels ◽  
El Alto ◽  
High Pollution

The traffic microenvironment accounts for a significant fraction of the total daily dose of inhaled air pollutants. The adverse effects of air pollution may be intensified in high altitudes (HA) due to increased minute ventilation (MV), which may result in higher deposition doses compared to that at sea level. Despite this, air quality studies in regions with combined high pollution levels and enhanced inhalation are limited. The main goals of this study are to investigate how the choice of travel mode (walking, microbus, and cable car ride) determines (i) the personal exposure to equivalent black carbon (eBC) and (ii) the corresponding potential respiratory deposited dose (RDD) in HA. For this investigation, we chose La Paz and El Alto in Bolivia as HA representative cities. The highest eBC exposure occurred in microbus commutes (13 μg m−3), while the highest RDD per trip was recorded while walking (6.3 μg) due to increased MV. On the other hand, the lowest eBC exposure and RDD were observed in cable car commute. Compared with similar studies done at sea level, our results revealed that a HA city should reduce exposure by 1.4 to 1.8-fold to achieve similar RDD at sea level, implying that HA cities require doubly aggressive and stringent road emission policies compared to those at sea level.

scholarly journals Modeling heavy metal release in the epiphytic lichen Evernia prunastri

2021 ◽  
Author(s):  
Andrea Vannini ◽  
Luca Paoli ◽  
Riccardo Fedeli ◽  
Sharon Kwambai Kangogo ◽  
Massimo Guarnieri ◽  
...  
Keyword(s):  
Heavy Metal ◽  
Remote Area ◽  
Metal Release ◽  
Evernia Prunastri ◽  
Epiphytic Lichen ◽  
Pollution Levels ◽  
Short Period ◽  
High Pollution ◽  
Heavy Metal Release ◽  
Very High

AbstractIn this study, the release of Cu2+ and Zn2+ was investigated and modeled in the epiphytic lichen Evernia prunastri. Samples were incubated with solutions containing these metals at ecologically relevant concentrations (10 and 100 μM) and then transplanted to a remote area and retrieved after 1, 2, 3, 6, 12, and 18 months. The results showed that, after 12 months, all samples faced similar metal reductions of ca. 80–85%, but after this period, all the involved processes seem to be no longer capable of generating further reductions. These results suggest that the lichen E. prunastri can provide information about environmental improvements after exposure to high or very high pollution levels in a relatively short period of time.

Changing markets – Medicinal plants in the markets of La Paz and El Alto, Bolivia

2016 ◽  
Vol 193 ◽  
pp. 76-95 ◽  
Author(s):  
Rainer W. Bussmann ◽  
Narel Y. Paniagua Zambrana ◽  
Laura Araseli Moya Huanca ◽  
Robbie Hart
Keyword(s):  
Medicinal Plants ◽  
La Paz ◽  
El Alto

Tensions between tiers of Bolivian government may grow

2021 ◽  
Keyword(s):  
National Level ◽  
Far Right ◽  
La Paz ◽  
Gubernatorial Elections ◽  
Content Type ◽  
Modus Vivendi ◽  
El Alto ◽  
The Government

Significance The MAS’s national-level appeal tends not to translate into support in localised elections, and a poor choice of candidates, particularly in El Alto, has proved self-defeating. Impacts Second-round gubernatorial elections will probably take place in six out of nine departments. Camacho, a far-right businessman turned politician, will use his newly gained legitimacy to harry the government. The Arce government will seek a modus vivendi with opposition mayors such as those of La Paz and Cochabamba.

Pulmonary gas exchange in humans exercising at sea level and simulated altitude

1986 ◽  
Vol 61 (1) ◽  
pp. 260-270 ◽  
Author(s):  
P. D. Wagner ◽  
G. E. Gale ◽  
R. E. Moon ◽  
J. R. Torre-Bueno ◽  
B. W. Stolp ◽  
...  
Keyword(s):  
Gas Exchange ◽  
Arterial Pressure ◽  
Sea Level ◽  
Pulmonary Arterial Pressure ◽  
Minute Ventilation ◽  
Statistical Significance ◽  
Random Order ◽  
Normal Subjects ◽  
Simulated Altitude ◽  
Pulmonary Arterial

In a previous study of normal subjects exercising at sea level and simulated altitude, ventilation-perfusion (VA/Q) inequality and alveolar-end-capillary O2 diffusion limitation (DIFF) were found to increase on exercise at altitude, but at sea level the changes did not reach statistical significance. This paper reports additional measurements of VA/Q inequality and DIFF (at sea level and altitude) and also of pulmonary arterial pressure. This was to examine the hypothesis that VA/Q inequality is related to increased pulmonary arterial pressure. In a hypobaric chamber, eight normal subjects were exposed to barometric pressures of 752, 523, and 429 Torr (sea level, 10,000 ft, and 15,000 ft) in random order. At each altitude, inert and respiratory gas exchange and hemodynamic variables were studied at rest and during several levels of steady-state bicycle exercise. Multiple inert gas data from the previous and current studies were combined (after demonstrating no statistical difference between them) and showed increasing VA/Q inequality with sea level exercise (P = 0.02). Breathing 100% O2 did not reverse this increase. When O2 consumption exceeded about 2.7 1/min, evidence for DIFF at sea level was present (P = 0.01). VA/Q inequality and DIFF increased with exercise at altitude as found previously and was reversed by 100% O2 breathing. Indexes of VA/Q dispersion correlated well with mean pulmonary arterial pressure and also with minute ventilation. This study confirms the development of both VA/Q mismatch and DIFF in normal subjects during heavy exercise at sea level. However, the mechanism of increased VA/Q mismatch on exercise remains unclear due to the correlation with both ventilatory and circulatory variables and will require further study.

Pulmonary gas exchange in humans during exercise at sea level

1986 ◽  
Vol 60 (5) ◽  
pp. 1590-1598 ◽  
Author(s):  
M. D. Hammond ◽  
G. E. Gale ◽  
K. S. Kapitan ◽  
A. Ries ◽  
P. D. Wagner
Keyword(s):  
Gas Exchange ◽  
Sea Level ◽  
Minute Ventilation ◽  
Normal Subjects ◽  
Inert Gas ◽  
Diffusion Limitation ◽  
O2 Uptake ◽  
Heavy Exercise ◽  
Blood Temperature ◽  
O2 Diffusion

Previous studies have shown both worsening ventilation-perfusion (VA/Q) relationships and the development of diffusion limitation during exercise at simulated altitude and suggested that similar changes could occur even at sea level. We used the multiple-inert gas-elimination technique to further study gas exchange during exercise in healthy subjects at sea level. Mixed expired and arterial respiratory and inert gas tensions, cardiac output, heart rate, minute ventilation, respiratory rate, and blood temperature were recorded at rest and during steady-state exercise in the following order: rest, minimal exercise (75 W), heavy exercise (300 W), heavy exercise breathing 100% O2, repeat rest, moderate exercise (225 W), and light exercise (150 W). Alveolar-to-arterial O2 tension difference increased linearly with O2 uptake (VO2) (6.1 Torr X min-1 X 1(-1) VO2). This could be fully explained by measured VA/Q inequality at mean VO2 less than 2.5 l X min-1. At higher VO2, the increase in alveolar-to-arterial O2 tension difference could not be explained by VA/Q inequality alone, suggesting the development of diffusion limitation. VA/Q inequality increased significantly during exercise (mean log SD of perfusion increased from 0.28 +/- 0.13 at rest to 0.58 +/- 0.30 at VO2 = 4.0 l X min-1, P less than 0.01). This increase was not reversed by 100% O2 breathing and appeared to persist at least transiently following exercise. These results confirm and extend the earlier suggestions (8, 21) of increasing VA/Q inequality and O2 diffusion limitation during heavy exercise at sea level in normal subjects and demonstrate that these changes are independent of the order of performance of exercise.

Diffusion limitation in normal humans during exercise at sea level and simulated altitude

1985 ◽  
Vol 58 (3) ◽  
pp. 989-995 ◽  
Author(s):  
J. R. Torre-Bueno ◽  
P. D. Wagner ◽  
H. A. Saltzman ◽  
G. E. Gale ◽  
R. E. Moon
Keyword(s):  
Sea Level ◽  
Minute Ventilation ◽  
Inert Gas ◽  
Diffusion Resistance ◽  
Diffusion Limitation ◽  
O2 Concentration ◽  
Normal Humans ◽  
Respiratory Gases ◽  
Arterial Po2 ◽  
Alveolar Capillary

The relative roles of ventilation-perfusion (VA/Q) inequality, alveolar-capillary diffusion resistance, postpulmonary shunt, and gas phase diffusion limitation in determining arterial PO2 (PaO2) were assessed in nine normal unacclimatized men at rest and during bicycle exercise at sea level and three simulated altitudes (5,000, 10,000, and 15,000 ft; barometric pressures = 632, 523, and 429 Torr). We measured mixed expired and arterial inert and respiratory gases, minute ventilation, and cardiac output. Using the multiple inert gas elimination technique, PaO2 and the arterial O2 concentration expected from VA/Q inequality alone were compared with actual values, lower measured PaO2 indicating alveolar-capillary diffusion disequilibrium for O2. At sea level, alveolar-arterial PO2 differences were approximately 10 Torr at rest, increasing to approximately 20 Torr at a metabolic consumption of O2 (VO2) of 3 l/min. There was no evidence for diffusion disequilibrium, similar results being obtained at 5,000 ft. At 10 and 15,000 ft, resting alveolar-arterial PO2 difference was less than at sea level with no diffusion disequilibrium. During exercise, alveolar-arterial PO2 difference increased considerably more than expected from VA/Q mismatch alone. For example, at VO2 of 2.5 l/min at 10,000 ft, total alveolar-arterial PO2 difference was 30 Torr and that due to VA/Q mismatch alone was 15 Torr. At 15,000 ft and VO2 of 1.5 l/min, these values were 25 and 10 Torr, respectively. Expected and actual PaO2 agreed during 100% O2 breathing at 15,000 ft, excluding postpulmonary shunt as a cause of the larger alveolar-arterial O2 difference than accountable by inert gas exchange.

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