Temperature Loggers Research Articles

Scalable Production of Self-Powered Printed Temperature Loggers Using Functional Inks

Scalable Production of Self-Powered Printed Temperature Loggers Using Functional Inks

전 주기 실시간 모니터링 시스템 구축에 관한 바이오의약품 운송 사례 연구

The cold chain monitoring market is drawing attention as regulations on drug transport are strengthened to maintain biopharmaceutical quality. The comprehensive temperature excursion management for biopharmaceutical distribution is inevitable in order to maintain the effectiveness and efficacy of them. For this reason, it is emphasized to establish the cold chain monitoring over the entire period, which is delivered from the place of origin to the customer. Immucell LC was selected as the subject of this research on the real-time monitoring system. The delivery processes of Immuncell LC can be divided into the process of manufacturing biologic agent from the blood culture of patient and the process of delivering it to the patient. This study aims to analyze the real case which is applied real-time monitoring system through the entire processes. In conclusion, it suggested the implications for improving work productivity, product stability and logistics management by analyzing transportation resources(packing materials, vehicles, carriers, temperature logger), logistics information systems, transportation procedures.

Термобиологические характеристики ушастых круглоголовок (Phrynocephalus mystaceus) (Reptilia, Agamidae) на бархане Сарыкум (Дагестан, Россия), полученные с помощью логгеров температуры

The paper compares two variants of thermobiological studies of toad-headed agamas (Phrynocephalus mystaceus) – the traditional one, based on route trapping and measurements of body temperature in captured lizards, and the new one, using temperature loggers that register body temperature once a minute and implemented interperitoneally. Both work options are not alternative. The main thing is the correct interpretation of the results: the traditional method provides data obtained from many individuals characterizing the temperature parameters of the activity of the studied reptiles. The new technique allows, although on a limited number of individuals, but with a huge number of measurements, to obtain the calculated characters of the reptiles' thermoregulation. Both of them successfully complement each other and, with subsequent refinement, could represent some single whole, allowing for a more complete and accurate understanding and description of the thermal biology of different reptile species.

Recent ground thermo-hydrological changes in a southern Tibetan endorheic catchment and implications for lake level changes

Abstract. Climate change modifies the water and energy fluxes between the atmosphere and the surface in mountainous regions such as the Qinghai–Tibet Plateau (QTP), which has shown substantial hydrological changes over the last decades, including rapid lake level variations. The ground across the QTP hosts either permafrost or is seasonally frozen, and, in this environment, the ground thermal regime influences liquid water availability, evaporation and runoff. Consequently, climate-induced changes in the ground thermal regime may contribute to variations in lake levels, but the validity of this hypothesis has yet to be established. This study focuses on the cryo-hydrology of the catchment of Lake Paiku (southern Tibet) for the 1980–2019 period. We process ERA5 data with downscaling and clustering tools (TopoSCALE, TopoSUB) to account for the spatial variability of the climate in our forcing data (Fiddes and Gruber, 2012, 2014). We use a distributed setup of the CryoGrid community model (version 1.0) to quantify thermo-hydrological changes in the ground during this period. Forcing data and simulation outputs are validated with data from a weather station, surface temperature loggers and observations of lake level variations. Our lake budget reconstruction shows that the main water input to the lake is direct precipitation (310 mm yr−1), followed by glacier runoff (280 mm yr−1) and land runoff (180 mm yr−1). However, altogether these components do not offset evaporation (860 mm yr−1). Our results show that both seasonal frozen ground and permafrost have warmed (0.17 ∘C per decade 2 m deep), increasing the availability of liquid water in the ground and the duration of seasonal thaw. Correlations with annual values suggest that both phenomena promote evaporation and runoff. Yet, ground warming drives a strong increase in subsurface runoff so that the runoff/(evaporation + runoff) ratio increases over time. This increase likely contributed to stabilizing the lake level decrease after 2010. Summer evaporation is an important energy sink, and we find active-layer deepening only where evaporation is limited. The presence of permafrost is found to promote evaporation at the expense of runoff, consistently with recent studies suggesting that a shallow active layer maintains higher water contents close to the surface. However, this relationship seems to be climate dependent, and we show that a colder and wetter climate produces the opposite effect. Although the present study was performed at the catchment scale, we suggest that this ambivalent influence of permafrost may help to understand the contrasting lake level variations observed between the south and north of the QTP, opening new perspectives for future investigations.

Temperature uncertainty modelling with proxy structural data as geostatistical constraints for well siting: an example applied to Granite Springs Valley, NV, USA

Utilizing existing temperature and structural geology information around Granite Springs Valley, Nevada, we build 3D stochastic temperature models with the aims of evaluating the 3D uncertainty of temperature and choosing between candidate exploration well locations. The data used to support the modelling are measured temperatures and structural proxies from 3D geologic modelling (distance to fault, distance to fault intersections and terminations, Coulomb stress change and dilation tendency), the latter considered ‘secondary’ data. Two stochastic geostatistical techniques are explored for incorporating the structural proxies: cosimulation and local varying mean. With both the cosimulation and local varying mean methods, many equally-likely temperature models (i.e. realizations) are produced, from which temperature probability profiles are calculated at candidate well locations. To aid in choosing between the candidate locations, two quantities summarize the temperature probabilities: V prior and entropy. V prior quantifies the likelihood for economic temperatures at each candidate location, whereas entropy identifies where new information has the most potential to reduce uncertainty. In general, the cosimulation realizations have smoother spatial structure, and extrapolate high temperatures at candidate locations that are located along the direction of the longest spatial correlation, which are down dip from existing temperature logs. The smooth realizations result in tight temperature probability profiles that are easier to interpret, but they have unrealistic temperature reversals in some locations because of the dipping ellipsoid shape created and that the cosimulation technique does not enforce a conductive geothermal gradient as a baseline (i.e. linearly increasing temperature with depth). The local varying mean results produce realizations with more realistic geothermal gradients, with temperatures increasing downward since a depth-temperature relationship is included. However, because they have much noisier spatial nature compared to cosimulation, it is harder to interpret the temperature probability profiles. The different local varying mean results allow the geologist to determine which proxy (e.g. dilation v. distance to fault termination) should be used given the specific geothermal system. In general, V prior from local varying mean results identify locations that are close to high values for the structural proxies: areas with higher probabilities for higher temperatures. The entropy results identify where uncertainty is greatest and therefore new drilling information could be most useful. Though these techniques provide useful information, even when applied to areas of sparse data, our comparison of these two techniques demonstrates the need for new geothermal geostatistics techniques that combine the advantages of these two methods and that are tailored to the spatial uncertainty issues inherent in geothermal exploration.

The vitality of native grassland plants in current urban climatic conditions in Gauteng, South Africa

Plants are essential components of urban microclimates, as they can help mitigate some of the adverse effects of urbanisation, enhance environmental quality, and thus contribute to overall species well-being and the sustainability of cities. Urban planners and policymakers often incorporate green infrastructure and urban greening into their strategies to create healthier and more livable urban environments. Plants are primary producers, serving as a baseline for the attraction and habitat of other species; they also provide vital ecosystem services, such as climate amelioration. Landscape designers and horticulturalists can influence plant selection through built environment interventions, increasing urban ecosystem services and benefits. Based on the evidence of native plant preferences by insects and people and their natural adaptation to regional climatic extremes, we tested, through an experimental study, the potential of native grassland plants to survive in assemblages in current urban environments. The study specifically monitored the tolerance of nine native grassland plant species to urban environments over six months in Gauteng, South Africa. A stratified random sampling was done by monitoring permanent quadrats in two purposefully engineered urban native gardens. Plant vitality was evaluated using chlorophyll a fluorescence. General climate data were obtained from a local weather station. Microclimatic temperature and humidity data were collected at each site and quadrat using Hygrochron High-Resolution Temperature and Humidity data loggers. The results indicated that all nine native plant species functioned with good photosynthetic health and can be recommended as resilient species that tolerate current urban conditions. Correlation studies indicated that two forb species, Haplocarpha lyrata and Scabiosa columbaria, showed great tolerance to current urban conditions. This vitality is likely contributed to their winter dormancy morphologically based on below-ground biomass, and their physiological adaptation to tolerate both wet and dry habitat conditions. This points to the potential of grassland forb species for urban use and the potential for climate adaptation in grassland areas.

Comparison of NDVI-2 Vaccine EID50 Titre Values After Three Weeks of Freight Under Cold Monitored Storage Condition

Abstract The EID50 titres per dose values of three batches of NDVI-2 were determined as log10 EID50 7.7, 7.6 and 6.8 after production, against reference EID50 5.5 per dose. These values were log10 EID50 2.2, 2.1 and 1.3 above the reference EID50 for NDVI-2. These vaccines were re-evaluated at PANVAC laboratory Debre-Zeit, prior to release. The initial EID50 values were compared with EID50 values obtained by the certifying laboratory, after three weeks of cold monitored freight. The packaged vaccine cold storage temperature of +1.9 oC prior to the shipment, was recorded with the aid of a temperature logger. The temperature logger was set to record and retain packaged vaccine cold storage temperature at hourly intervals during the freight. At the end of three-week freight, the temperature logger readings were analysed, and temperature range of -2.48 oC to 7.7 oC was observed throughout the freight. However, sudden rise in packaged vaccine storage temperature from 7.7 oC to 22.28 oC was noticed on the last day of freight. The initial EID50 titre per dose values, when compared with EID50 log10 6.5, 6.8, and 6.6 per dose obtained by the certifying laboratory after the cold monitored freight and re-evaluation, showed EID50 titre loss of log10 EID50 1.2, 0.8 and 0.6, respectively. The observed EID50 loss could not invalidate these vaccine batches, considering that these had an initial EID50 titre per dose values that were well above the reference EID50 titre for NDVI-2. In Nigeria, and to our knowledge, this is the first recorded monitored cold storage temperature transit for NDVI-2.

Design and validation of an open-sourced automation system for vertical farming

The Modular Automated Crop Array Online System (MACARONS) is a scalable, customisable and open-sourced platform designed for plant care, monitoring, and transportation. It offers specific dosing for individual plants, automated data logging of temperature, humidity, and images, and custom behaviours programmable in Python. Monitoring and control of the system is achieved through a web-interface. The system was validated by autonomously caring for five lettuce plants over a five-week period. This was done indoors under artificial lighting and uncontrolled ambient conditions. The system is estimated to perform the tasks required 30% faster than a human operator and can handle payloads of up to 5 kg with a maximum footprint of 750 mm × 500 mm. The validated system supports 12 payloads and can be easily scaled to accommodate more. The designs are released and meets the requirements of CERN-OSH-W, which includes step-by-step graphical build instructions and can be built at a cost of GBP 2241.72 (USD 2793.82). The system aims to provide cost-effective automation to reduce labour costs and provide precise control of irrigation and nutrients. The current system is limited by the dosing time and the space-use efficiency. We provided future directions and modifications that can be made to address this.

A disposable reader-sensor solution for wireless temperature logging

A disposable reader-sensor solution for wireless temperature logging

1429. Temperature and Humidity Variations in the Operating Room: A Risk Assessment

Abstract Background The American Society of Heating, Refrigeration, and Air-Conditioning Engineers (ASHRAE) recommends that hospital operating rooms (OR) are controlled for temperature and humidity with established ranges but does allow for exceedances for surgeons and surgical procedures. There is currently no clear consensus or established thresholds for out-of-range temperature and humidity ranges in relation to risk for surgical site infections (SSI). A study was performed at Memorial Sloan Kettering Cancer Center (MSKCC) to further examine if temperature and humidity deviations pose a patient safety risk. Methods The study included 5600 surgical procedures that were performed at MSKCC between September 2021 and January 2022 where temperature and humidity logs were available. Procedures were broken into groups based on in- (n=4419) and out-of-range (n=1187) temperatures and in- (n=5225) and out-of-range (n=381) humidity. SSIs following the procedure were identified using targeted positive microbiology cultures and within NHSN (National Healthcare Safety Network) surveillance periods. Chi-square and Fisher’s exact statistical tests were used to determine if there was a significant difference between groups where p < 0.05. Breakdown of eligible procedures and follow up Table represents the total number of eligible procedures with environmental parameters and SSI follow up period. Results There was no significant impact on SSI for out-of-range humidity (p=0.15). There was a significantly higher SSI rate observed for out-of-range temperatures (p=0.04) more specifically low out- of-range temperatures (p=0.02). A sub-analysis was performed for low temperatures based on procedures by duration. Significance of the finding was lost when surgery duration was 4 hours or greater. Conclusion If there was a true correlation between SSI and low ambient temperature, we would have expected to see a strengthening of SSI risk with longer procedures. This study suggests that temperature and humidity deviations out of the recommended guidelines in the operating room do not pose additional risks for surgical site infections and limited exceedances can be permitted without risking patient safety. Disclosures All Authors: No reported disclosures

Thermal structure of two deep boreholes in the Siljan Ring, Central Sweden, and palaeoclimatic implications

Heat-flow data from deep boreholes are of particular value as a number of factors, including climatic surface temperature variations, may disturb subsurface thermal conditions, especially at shallow depths. This study provides thermal results from two boreholes, Gravberg-1 and Stenberg-1, drilled to large depths in the Siljan Ring impact structure, Baltic Shield, Central Sweden. Taking several high-resolution temperature logs to a depth of more than 5000 m in Gravberg-1 and close to 2000 m in Stenberg-1, and up to a long time after drilling, ensures high-quality deep temperature data. A good-quality thermal conductivity profile was determined from mineralogical composition and radiogenic heat production from a spectral gamma-ray log. The observations show overall thermal conductive profiles with local non-conductive temperature variations. Observed present-day near-surface heat flow (depth range 200–500 m) in Gravberg-1 is 47 mW/m2 (std. dev. 1.5 mW/m2). From observed deep background heat flow, considering heat production, the equivalent steady-state, unperturbed heat flow is estimated at 66–68 mW/m2. Data from Stenberg-1 provide similar results. The observed reduction of heat flow at near-surface level by about 20 mW/m2 is interpreted as originating from long-term palaeoclimatic temperature variations. During the last glacial period, the area was, to varying degree, both ice-free and covered by the Fennoscandian ice sheet. Thermal modelling, with a ground-surface mean-temperature increase by 12±2 °C from glacial to post-glacial time, shows consistency between observed and modelled heat flow perturbations for the full depth range of observations. Heat flow perturbations may be significant to depths of about 2000 m. These results show that, uncorrected for palaeoclimate, depending on depths of measurements, observed continental heat flow values might be markedly underestimated. This applies to Northern Europe and, likely, to many other areas as well.

Measurement of wellbore leakage in high‐pressure gas well based on the multiple physical signals and history data: Method, technology, and application

AbstractLeakage is one of the most serious challenges for the safe production of high‐pressure gas wells for its high risks, including abnormal annular pressure, natural gas accumulation, and environment pollution, but available methods can hardly accurately measure the leakage type and depth, which are the key parameters for the rigless leakage repair and risk assessment. Therefore, this paper proposes a method to measure the leakage based on the characteristics, which combines qualitative and quantitative measurement together. Qualitative measurement considers the annular pressure, tubing pressure, liquid level, cement quality, and workover history. Quantitative measurement is determined by noise logging, electromagnetic logging, pressure logging, and temperature logging. The logging should be optimized according to the qualitative measurement. The method was successfully applied in high‐pressure gas well belonging to Tarim Oilfield. Two potential leakage types are provided based on the annular pressure, liquid level, cement quality, and workover history, including tubing leakage and linger hanger leakage. Based on the potential leakage types, the pressure difference, logging devices string, stopping length, and time are optimized to make the engineering logging reliable. Through measurement, two leakage points are found in tubing string. One is tubing body crack at the depth of 2724 m and the other is tubing thread leakage at the depth of 5211.7 m, which well matches the production data.

Technique and results of determination of vertical variations in rock thermal properties, temperature gradient and heat flow

The paper describes the results of experimental geothermal studies of the formation surrounding Savitskaya-300 well (depth 3555 m) drilled in the Volga-Ural oil and gas basin (Orenburg region, Russia). The work was aimed, firstly, at obtaining geothermal data for basin modeling and, secondly, at improving the instrumental and methodological foundations of experimental studies. Continuous core profiling of the rock thermal conductivity, volumetric heat capacity, and thermal anisotropy was performed on all 2886 recovered core samples with the total length of 329.1 m. Additional measurements were conducted at fluid saturation and elevated temperatures. For non-cored intervals, the rock thermal properties were determined from well-logging data and via measurements on rock cuttings. The studied formation is characterized by high thermal heterogeneity at both the level of strata (horizons) and individual samples. Significant thermal anisotropy up to 1.50–1.66 in the lower part of the well has been observed. To obtain data on vertical variations of equilibrium temperature and its gradient, temperature logging was performed 7 times within the 2 to 186 days of well shut-in. New data on the recovery of temperature and its gradient after drilling are important for the practice of applied and fundamental geothermal surveys. A significant increase in heat flow with depth was established based on the results of temperature gradient and rock thermal conductivity determination for 34 depth intervals. The observed general vertical variation in the whole depth range of the well up to ∼3.3 km depth can be attributed to paleoclimatic effect in the Late Pleistocene-Holocene, while the sharp increase in heat flow at ∼3.3 km within Fransian sediments is possibly due to advective heat transfer by fluid filtration. The apparent heat flow was established to be 84.3 mW⋅m−2 in the lower section of the well, below 3.3 km. The value may be close to the steady-state heat flow value, which is 84% higher than the previous published average data for the studied area.

165 Evaluation of the Use of Prenatal Immune Stimulation on the Ability to Alter Postnatal Immune Function in Weaned Pigs

Abstract One of the most lacking areas where improvements can be made in swine production is in the area of swine health. This study was designed to determine whether exposure to low dose endotoxin (lipopolysaccharide; LPS) during gestation can enhance immunity to a subsequent LPS challenge in piglets after weaning. Pregnant Camborough sows (parity: 2.6 ± 1.4) were assigned to prenatal immune stimulation (LPS; n = 7; administered 2.5 µg/kg BW LPS i.m. at d 78 ± 1.8 of gestation) or saline treatment groups (CON; n = 7). From the 2 prenatal treatment groups, barrows (n = 17 LPS, 17 CON) were identified at weaning (21 ± 1.3 d of age) to subsequently receive a post-weaning LPS challenge. On d -7, barrows were transported to the USDA-ARS Livestock Issues Research Unit in Lubbock, TX where they were housed in individual pens in an environmentally controlled building with ad libitum access to water and a starter ration. On d -1, pigs were fitted with indwelling jugular catheters and subcutaneous temperature loggers. On d 0, pigs were challenged i.v. with LPS (10 µg/kg BW) and blood samples were collected at -2, 0, 1, 2, 4, 6, 8, 12, and 24 h relative to LPS challenge. Data were analyzed using PROC MIXED in SAS, specific for repeated measures. There was a treatment × time interaction for subcutaneous temperature (P < 0.01), where temperature increased more quickly at 1 and 2 h post-challenge in LPS compared with CON pigs. There was a tendency (P = 0.08) for less change in white blood cells, relative to baseline values, in LPS compared with CON pigs. There was a treatment × time interaction (P = 0.01) for lymphocyte concentrations where concentrations were reduced in LPS compared with CON pigs at 8 h post-challenge. There was also a treatment × time interaction (P = 0.01) for the change in eosinophil concentrations, where there was less change in eosinophil concentrations from 1 to 12h in LPS compared with CON pigs. There was a tendency (P = 0.08) for a treatment × time interaction for serum interleukin-6 (IL-6), where concentrations were reduced in LPS compared with CON pigs at 2h (P = 0.01) and tended to be reduced at 1 and 4h post-challenge (P ≤ 0.11). There was a tendency (P = 0.06) for a treatment × time interaction for IL-8, where concentrations were reduced in LPS compared with CON pigs at 1 and 4h (P ≤ 0.01) and tended to be reduced at 2h post-challenge (P = 0.06). Granulocyte macrophage colony stimulating factor and tumor necrosis factor-α tended (P ≤ 0.08) to be reduced in LPS compared with CON pigs. These data suggest that exposure to endotoxin in utero can influence the postnatal innate immune response to endotoxin. Thus, it is possible to influence the innate immune response of pigs in utero, which may serve as a method to positively influence postnatal immune responsiveness.

Exploratory analysis of the operation of a MHRV system in an overheating nZEB apartment in Spain

This article investigates the operation of a Mechanical Heat Recovery Ventilation (MHRV) system in an overheating nZEB apartment in Spain. The building, an apartment tower, was found to have a moderate to severe issue of overheating during extensive parts of the year. The study focuses on a flat located on the top floor of the Bolueta tower I in Bilbao, Spain, which is the world’s tallest Passivhaus building. Temperature and relative humidity data loggers were placed in various locations inside and outside the flat, as well as an amperemeter to monitor the operating regime of the MHRV unit’s fans. The study covered a period of 18 months and consisted in an exploratory analysis of the data obtained. The results show that the dwelling and its ventilation system partially correspond to the expected performance during the cold season but deviate from the usual design assumptions considered for the warm periods. The MHRV unit may have difficulties entering bypass mode and providing sufficient free cooling to maintain adequate indoor temperatures due to its placement. These findings provide insight into the thermal performance of the building and operation of the MHRV system and can inform future research.

Headwater stream temperature response to forest harvesting: Do lower flows cause greater warming?

AbstractThis study addressed two hypotheses regarding the relationship between stream temperature response to shade removal and streamflow: (a) that temperature response increases as flow declines and (b) that the relationship can be complicated by shifts in dominant streamflow sources and pathways during low‐flow periods. The study was based on a paired‐catchment design in rain‐dominated headwater catchments in the southern Coast Mountains of British Columbia, Canada, and focused on the effect of a 50% thinning treatment on daily maximum temperature in June, July and August for three sites within the harvest treatment. At the two upstream sites, the treatment response exhibited a negative relationship with daily mean streamflow, especially for days with high incident solar radiation. This result suggests that the effectiveness of forest practice rules for protecting cold‐water habitat may be reduced under future climatic conditions characterized by more frequent extended drought. However, stream temperature response at the most downstream site exhibited a pronounced inverted‐U‐shaped relationship with streamflow measured at a weir. It is hypothesized that the response at the most downstream temperature logger was controlled by the existence of a stable, relatively cool inflow just upstream of the logger, which represented an increasing fraction of flow as streamflow generated higher up in the catchment declined through time. There was a lack of convergent surface topography upstream of the logger, and it is hypothesized that localized inflow may have been controlled by the topography of the soil‐till interface and/or originated as hyporheic discharge.

34 Assessing the Ability to Immunomodulate the Innate Immune System and Oxidative Status of Weaned Pigs Through a Prenatal Lipopolysaccharide Challenge

Abstract Gastrointestinal immunity and antioxidant defenses may be bolstered in young animals through prenatal immune system stimulation (PIS), but this is largely uninvestigated in swine. The objective of this experiment was to determine if a low dose of lipopolysaccharide (LPS) administered to late-gestating sows would alter the immune response and oxidative status of subsequent offspring. On d 78 ± 1.8 of gestation, 14 Camborough sows (Parity = 2.6±1.4) of the same farrowing group were blocked by body weight and randomly assigned to one of two treatments: intramuscular injection of saline (CON) or LPS from E. coli O111:B4 (2.5 µg/kg of BW). Sow rectal temperatures (RT) and sickness behavior scores (SBS) were recorded every 0.5 h from -0.5 h to 8 h and every 8 h from 8 to 48 h post-treatment. A subset of 34 weaned barrows (n = 17 CON, LPS; weaning age 21 ± 1.3 d) from the experimental sow group were transported on d -7 to an environmentally controlled facility where they were individually housed with ad libitum access to water and feed. On d -1, pigs were anesthetized for placement of a subcutaneous temperature logger and a jugular catheter. On d 0, all pigs were challenged intravenously with the same LPS strain (10 µg/kg of BW) previously administered to sows. Body temperature was measured at 5-min intervals from the time of logger placement. Blood samples were collected at -2, 0, 1, 2, 4, 6, 8, 12, and 24 h relative to LPS administration at 0 h. After the 24 h blood collection, pigs were necropsied for ileal and jejunal tissue. Plasma samples, jejunal and ileal tissues were analyzed for total antioxidant capacity (TAC) and malondialdehyde (MDA). Data were analyzed as a linear mixed model using PROC MIXED (SAS 9.4) with treatment and time as fixed effects. A dependent covariance structure was used for repeated measurements. Sows administered LPS had elevated RT from 2 to 16-h post-challenge with return to baseline by h 24, indicating mild immune stimulation (treatment × time; P < 0.01). Similarly, sows exposed to LPS had increased SBS from 2 to 3.5 h post-challenge (treatment × time; P < 0.01). Pigs exposed to PIS had greater body temperature than CON at 1 and 2 h post-LPS (treatment × time; P < 0.01). An increase in plasma TAC at 2 and 4 h post-LPS was observed in pigs exposed to PIS relative to CON (treatment × time; P < 0.01). Irrespective of treatment, LPS increased plasma MDA from 2 to 24 h post-challenge (time; P < 0.01). There was no effect of PIS on ileal or jejunal tissue TAC (P ≥ 0.40), but weaned pigs exposed to PIS had decreased jejunal MDA (P < 0.05). Collectively, it appears PIS may alter the innate immune response and oxidative status of the weaned pig during LPS challenge.

Melanistic coloration does not influence thermoregulation in the crepuscular gecko Eublepharis macularius.

Body coloration in ectotherms serves multiple biological functions, including avoiding predators, communicating with conspecific individuals, and involvement in thermoregulation. As ectotherms rely on environmental sources of heat to regulate their internal body temperature, stable melanistic body coloration or color change can be used to increase or decrease heat absorption and heat exchange with the environment. While the function of melanistic coloration for thermoregulation increases solar radiation absorption for heating in many diurnal ectotherms, research on crepuscular and nocturnal ectotherms is lacking. Since crepuscular and nocturnal ectotherms generally absorb heat from the substrate, in these organisms melanistic coloration may have other primary functions beside thermoregulation. As such, in this work we hypothesized that the proportion of dorsal melanistic body coloration would not influence heating and cooling rates in the crepuscular gecko, Eublepharis macularius, and that changes in environmental temperature would not trigger color changes in this species. Temperature measurements of the geckos and of the environment were taken using infrared thermography and temperature loggers. Color data were obtained using objective photography and a newly developed custom software package. We found that body temperature reflected substrate temperatures, and that the proportion of melanistic coloration has no influence on heating or cooling rates or on color changes. These findings support that melanistic coloration in E. macularius may not be used for thermoregulation and strengthen the hypothesis that in animals active in low light conditions, melanistic coloration may be used instead for camouflage or other functions.

An inexpensive method for reliable recovery of stream temperature data

AbstractObjectiveWater temperature is perhaps the single‐most important environmental driver of fish populations. The strong relationship between fish and water temperature allows fisheries managers to make predictions about the influence of temperature on fishes under both current and future climatic conditions. These predictions are more robust if based on year‐round and long‐term data. However, water temperature data are commonly compromised or lost altogether when data‐logging temperature sensors are damaged or go missing. In recognition of the need for reliable ways to collect long‐term, year‐round temperature data, we designed, implemented, and tested a durable but cryptic logger deployment and retrieval system.MethodsWe used metal housings and stakes to protect and anchor temperature loggers on the streambed and, when necessary, used a metal detector to assist with logger recovery. We then evaluated logger recovery rates across 12 years and 312 deployments at 85 sites in first‐ to ninth‐order Rocky Mountain streams and rivers.ResultAlthough we recovered only 73% of loggers with traditional means of retrieval (e.g., GPS or photo), presumably owing to the inconspicuous nature of our metal housings and streambed anchor stakes, we recovered 96% of loggers when a metal detector was also used. Ordinal and binary logistic regression revealed that a metal detector was especially beneficial when trying to recover loggers from unfamiliar monitoring sites or those deployed for long periods of time (years).ConclusionOur methods could be replicated for a reliable and inexpensive approach to acquiring year‐round stream temperature data.

High spatial resolution long-term temperature profiling to inform near-shore atmospheric sound propagation

Atmospheric sound propagation depends on factors such as surface characteristics and meteorological parameters. Effective numerical modeling of atmospheric sound propagation requires reliable and realistic input parameters. One of the most influential factors is the air temperature profile. This work examines the application of experimentally determined air temperature profiles in acoustic modeling of littoral environments. Long term measurements of near-surface air temperature profiles over water and marsh grass are presented. Data have been recorded using temperature loggers affixed to two permanent 7 m masts. The loggers were positioned with a 1 m vertical spacing. A common approach to characterize the near-surface boundary layer uses Monin–Obukhov Similarity Theory (MOST). This work compares high spatial resolution air temperature measurements with measurement-informed profiles based on MOST. The development of a more experimentally grounded set of assumptions will ultimately contribute to the improvement of atmospheric acoustic transmission loss models in near shore environments.