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Artykuły w czasopismach na temat „Moisture profile”

Autor: Grafiati

Data publikacji: 3 czerwca 2025

Data aktualizacji: 31 lipca 2025

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1

Tran, A. P., M. Vanclooster, and S. Lambot. "Improving soil moisture profile reconstruction from ground-penetrating radar data: a maximum likelihood ensemble filter approach." Hydrology and Earth System Sciences 17, no. 7 (2013): 2543–56. http://dx.doi.org/10.5194/hess-17-2543-2013.

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Abstract. The vertical profile of shallow unsaturated zone soil moisture plays a key role in many hydro-meteorological and agricultural applications. We propose a closed-loop data assimilation procedure based on the maximum likelihood ensemble filter algorithm to update the vertical soil moisture profile from time-lapse ground-penetrating radar (GPR) data. A hydrodynamic model is used to propagate the system state in time and a radar electromagnetic model and petrophysical relationships to link the state variable with the observation data, which enables us to directly assimilate the GPR data.

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2

Tran, A. P., M. Vanclooster, and S. Lambot. "Improving soil moisture profile prediction from ground-penetrating radar data: a maximum likelihood ensemble filter approach." Hydrology and Earth System Sciences Discussions 10, no. 2 (2013): 1581–615. http://dx.doi.org/10.5194/hessd-10-1581-2013.

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Abstract. The vertical profile of root zone soil moisture plays a key role in many hydro-meteorological and agricultural applications. We propose a closed-loop data assimilation procedure based on the maximum likelihood ensemble filter algorithm to update the vertical soil moisture profile from time-lapse ground-penetrating radar (GPR) data. A hydrodynamic model is used to propagate the system state in time and a radar electromagnetic model to link the state variable with the observation data, which enables us to directly assimilate the GPR data. Instead of using the surface soil moisture only

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3

Rosenkilde, A., and P. Glover. "High Resolution Measurement of the Surface Layer Moisture Content during Drying of Wood Using a Novel Magnetic Resonance Imaging Technique." Holzforschung 56, no. 3 (2002): 312–17. http://dx.doi.org/10.1515/hf.2002.050.

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Summary The moisture content profile in the surface layer of Scots pine (Pinus sylvestris) sapwood has been measured using the MRI (Magnetic Resonance Imaging) technique.Anovel high-gradient permanent magnet was used for the measurement of the moisture profile in the wood during the drying process, giving a depth resolution of better than 20 μm. This paper demonstrates for the first time the possibility of measuring the moisture content depth profile in the surface layer from raw state down to 4% moisture content without removing the wood sample from the apparatus. The main advantage of this t

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4

Heshmati, Sina, Mohammad Mazloomi, and Philip Evans. "Optimizing Surface Micro Grooving to Reduce the Checking and Cupping of Douglas Fir, Western Hemlock and White Spruce Decking Exposed to Natural Weathering." Journal of Manufacturing and Materials Processing 2, no. 4 (2018): 67. http://dx.doi.org/10.3390/jmmp2040067.

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Machining grooves into the surface of pine and fir (Abies spp.) deckboards reduces undesirable checking that develops when “profiled” boards are exposed to the weather. We aim to develop improved profiles for Douglas fir, western hemlock and white spruce decking to reduce their susceptibility to checking, and understand how profile geometry influences the stresses that cause checking. We varied the width and depth of grooves in profiled deckboards, exposed deckboards to the weather, and measured checking and cupping of boards. A numerical model examined the effect of groove depth on the moistu

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5

Starks, Patrick J., Gary C. Heathman, Thomas J. Jackson, and Michael H. Cosh. "Temporal stability of soil moisture profile." Journal of Hydrology 324, no. 1-4 (2006): 400–411. http://dx.doi.org/10.1016/j.jhydrol.2005.09.024.

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6

Groves, James R. "A PRACTICAL SOIL MOISTURE PROFILE MODEL." Journal of the American Water Resources Association 25, no. 4 (1989): 875–80. http://dx.doi.org/10.1111/j.1752-1688.1989.tb05403.x.

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7

Benáková, Martina, Tereza Kulovaná, and Miloš Jerman. "Moisture Migration in High Strength Concrete." Advanced Materials Research 982 (July 2014): 63–67. http://dx.doi.org/10.4028/www.scientific.net/amr.982.63.

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Moisture transport in high strength concrete is investigated in this paper. The experiment that involves the water suction is carried out in a long-term. The moisture profiles are measured by non-destructive capacitance method, the last profile is determined gravimetrically. The suction experiment is carried out in isothermal condition at the temperature of 22±1 °C and 25-30% relative humidity.

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8

Tian, Jie, Zhibo Han, Heye Reemt Bogena, et al. "Estimation of subsurface soil moisture from surface soil moisture in cold mountainous areas." Hydrology and Earth System Sciences 24, no. 9 (2020): 4659–74. http://dx.doi.org/10.5194/hess-24-4659-2020.

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Abstract. Profile soil moisture (SM) in mountainous areas is important for water resource management and ecohydrological studies of downstream arid watersheds. Satellite products are useful for providing spatially distributed SM information but only have limited penetration depth (e.g., top 5 cm). In contrast, in situ observations can provide measurements at several depths, but only with limited spatial coverage. Spatially continuous estimates of subsurface SM can be obtained from surface observations using multiple methods. This study evaluates methods to calculate subsurface SM from surface

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9

Blommaert, Anke, Marijke Steeman, and Nathan Van Den Bossche. "Modeling Moisture Accumulation and Decay Potential in Cross-Laminated Timber Wall Assemblies Exposed During the Construction Phase." Buildings 15, no. 7 (2025): 1075. https://doi.org/10.3390/buildings15071075.

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This study examines decay risks in cross-laminated timber (CLT) wall assemblies with built-in moisture, aiming to develop a simulation-based methodology to assess moisture dynamics during the construction phase. Differing from previous research, this study focuses on the central regions of CLT wall panels. Moisture distribution within the panel, especially in the exposed layer, is critical for understanding potential degradation. A series of simulations were conducted to determine the necessary level of detail for moisture profiling, comparing approaches that use a single average value, layer-

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10

Priadi, Trisna, and Gunes T. W. Giyarto. "Profil Suhu dan Kadar Air Kayu dalam Pengeringan Oven Pemanas dan Gelombang Mikro (Temperature and Moisture Content Profiles of Woods in Heating and Microwave Ovens Drying)." Jurnal Ilmu dan Teknologi Kayu Tropis 17, no. 2 (2021): 160–71. http://dx.doi.org/10.51850/jitkt.v17i2.517.

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This research aimed to evaluate the profile of temperature and moisture content in Pinus oocarpa wood being dried with heating oven and microwave oven. The size of samples were (25x70x120) mm3. The temperature profiles in heating oven and microwave oven drying were taken every 10 minutes and 0.5 minutes, respectively. The moisture profiles in heating oven and microwave oven drying were made in every 24 hours and 10 minutes, respectively. The heating oven was set at 60 °C, while microwave oven was set for 2 minutes intermittently with 5 minutes break. In microwave drying, the temperature inside

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11

DU, HONG SHUANG, CHENGYUAN LI, and CHUN WON KANG. "MEASURING THE ELECTRIC RESISTANCE OF AIR DRYING THICK RED PINE AND LARCH TIMBER." WOOD RESEARCH 67(5) 2022 67, no. 5 (2022): 866–74. http://dx.doi.org/10.37763/wr.1336-4561/67.5.866874.

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The objective of this study was to evaluate the moisture profile and drying period of air drying the red pine and Japanese larch timbers with the cross section of 14.0 cm × 14.0cm and16.5 cm × 16.5cmby measuring the electricresistanceofthe wood. The drying curvesdetermined by measuring electricresistanceand by oven-dried method were nearly identical at last drying stage, and had almost same moisture profiles and same drying period after the end of air drying. Therefore, the drying curve determined by measuring electricresistancecan be used to predict the drying period and moisture profile of a

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12

Graeff, T., E. Zehe, S. Schlaeger, et al. "A quality assessment of spatial TDR soil moisture measurements in homogenous and heterogeneous media with laboratory experiments." Hydrology and Earth System Sciences Discussions 7, no. 1 (2010): 269–311. http://dx.doi.org/10.5194/hessd-7-269-2010.

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Abstract. Investigation of transient soil moisture profiles yields valuable information of near- surface processes. A recently developed reconstruction algorithm based on the telegraph equation allows the inverse estimation of soil moisture profiles along coated, three rod TDR probes. Laboratory experiments were carried out to prove the results of the inversion and to understand the influence of probe rod deformation and solid objects close to the probe in heterogonous media. Differences in rod geometry can lead to serious misinterpretations in the soil moisture profile but have small influenc

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13

Graeff, T., E. Zehe, S. Schlaeger, et al. "A quality assessment of Spatial TDR soil moisture measurements in homogenous and heterogeneous media with laboratory experiments." Hydrology and Earth System Sciences 14, no. 6 (2010): 1007–20. http://dx.doi.org/10.5194/hess-14-1007-2010.

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Abstract. Investigation of transient soil moisture profiles yields valuable information of near- surface processes. A recently developed reconstruction algorithm based on the telegraph equation allows the inverse estimation of soil moisture profiles along coated, three rod TDR probes. Laboratory experiments were carried out to prove the results of the inversion and to understand the influence of probe rod deformation and solid objects close to the probe in heterogeneous media. Differences in rod geometry can lead to serious misinterpretations in the soil moisture profile, but have small influe

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14

Rokich, Deanna P., Kathy A. Meney, Kingsley W. Dixon, and K. Sivasithamparam. "The impact of soil disturbance on root development in woodland communities in Western Australia." Australian Journal of Botany 49, no. 2 (2001): 169. http://dx.doi.org/10.1071/bt00015.

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The impact of soil disturbance of the Banksia woodland soil profile and particularly the effect of different reconstructed soil profiles (overburden profile, white profile and yellow profile) and soil ripping within rehabilitation sites, was investigated in terms of root development and architecture for eight species that are key structural elements in Banksia woodland. The aim was to determine the soil environment best suited for root development and architecture likely to contribute to high seedling survival in post-mined sites. Root development and architecture differed significantly betwee

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15

Talebi, A., R. Uijlenhoet, and P. A. Troch. "Soil moisture storage and hillslope stability." Natural Hazards and Earth System Sciences 7, no. 5 (2007): 523–34. http://dx.doi.org/10.5194/nhess-7-523-2007.

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Abstract. Recently, we presented a steady-state analytical hillslope stability model to study rain-induced shallow landslides. This model is based on kinematic wave dynamics of saturated subsurface storage and the infinite slope stability assumption. Here we apply the model to investigate the effect of neglecting the unsaturated storage on the assessment of slope stability in the steady-state hydrology. For that purpose we extend the hydrological model to compute the soil pore pressure distribution over the entire flow domain. We also apply this model for hillslopes with non-constant soil dept

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16

Barneto, Agustin García, and J. Ariza Carmona. "Moisture profile determination in urea prill. I." Journal of the Science of Food and Agriculture 87, no. 12 (2007): 2217–21. http://dx.doi.org/10.1002/jsfa.2934.

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17

Koryakovskaya, Nataliya V., and Oksana I. Bederdinova. "Monitoring and Control of Paper Web Moisture." Lesnoy Zhurnal (Forestry Journal), no. 1 (February 1, 2022): 188–204. http://dx.doi.org/10.37482/0536-1036-2022-1-188-204.

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Product quality is a key indicator of the positive outcome of pulp and paper production. Moisture content is one of the main paper quality characteristics. The moisture profile across the paper web width shows possible shortcomings of the process equipment which, if corrected, will improve the consumer properties of paper and enhance economic efficiency. The research aims to assess whether the moisture content measurement results meet the requirements of the process regulations in the steady-state and transient modes of paper machine operation as well as the uniformity of the moisture profile

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18

Hashiguchi, Koji, Daniel Lisak, Agata Cygan, Roman Ciuryło, and Hisashi Abe. "Spectral analysis of H₂O near 7180 cm^–1 to accurately measure trace moisture in N₂ gas: evaluation of line shape profiles using Akaike Information Criterion." Japanese Journal of Applied Physics 61, no. 1 (2021): 012003. http://dx.doi.org/10.35848/1347-4065/ac3724.

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Abstract The absorption spectra of H2O in N2 gas were measured at atmospheric pressure and room temperature near 7180 cm–1 in the moisture range of 9.7–148.7 nmol mol−1 in mole fraction using cavity ring-down spectroscopy. The line shape profiles used for the spectral analysis for the trace moisture measurement were evaluated based on the Akaike Information Criterion as well as the fitting residuals. The optimal line shape profile in this study was the speed-dependent asymmetric Voigt profile (SDAVP). From the comparison of the fitting results calculated using the Lorentzian profile (LP) with

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19

Acworth, R. I., R. R. Young, and A. L. Bernadi. "Monitoring soil moisture status in a Black Vertosol on the Liverpool Plains, NSW, using a combination of neutron scattering and electrical image methods." Soil Research 43, no. 2 (2005): 105. http://dx.doi.org/10.1071/sr04064.

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Electrical image data were used to estimate soil moisture content beneath smectite-dominated black Vertosol in the Liverpool Plains catchment in northern New South Wales. Measurements carried out over a range of soil moisture conditions included: water use by lucerne sown into a full profile, recharge of profiles after lucerne and long fallow after a cereal crop. Measurements were repeated approximately every 2 months between September 2000 and August 2001. Estimates of bulk electrical conductivity (EC), determined from inversion of apparent conductivity electrical images, were compared to soi

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20

Bhattacharyya, Pratap, R. Yadav, Ram Prasad, R. Aggarwal, and Pratap Singh. "Water balance and growth parameters of three important forest tree species of Shivalik foothills in Haryana." Indian Journal of Forestry 30, no. 3 (2007): 299–305. http://dx.doi.org/10.54207/bsmps1000-2007-n79bw2.

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Based on rainfall, interception, runoff, evapotranspiration, capillary contribution, deep percolation and soil moisture storage in 1.5 m profile, water balance of three forest species namely, Acacia nilotica, Dalbergia sissoo and Leucaena leucocephala was estimated for the months during 2003-04, in their initial growth stage in fragile Shivalik foothill of Haryana. All these species survived well with 80-100 per cent survival rate. It has been found that all the three species extracted moisture up to 90 cm depth in initial 2-3 years of growth. Deep percolation losses from 1.5 m profile were si

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21

Bae, Abraham, Shelley M. Stoffels, Charles E. Antle, and Seung Woo Lee. "Observed evidence of subgrade moisture influence on pavement longitudinal profile." Canadian Journal of Civil Engineering 35, no. 10 (2008): 1050–63. http://dx.doi.org/10.1139/l08-047.

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The relationship between subgrade moisture parameters and pavement profile was explored for 34 asphalt pavements of the seasonal monitoring program (SMP) in the long-term pavement performance (LTPP) program. Volumetric moisture content was quantified in terms of the moisture index (MI), representing moisture as reasonably related to subgrade performance. Using power spectral density (PSD), roughness was evaluated in 21 individual wavebands. From statistical analysis, it was concluded that subgrade moisture significantly affects roughness in the wavebands of 14.9 to 31.2 m and 24.0 to 31.2 m fo

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22

R. SAHA and V.K. MISHRA. "Estimation of profile moisture status from surface moisture in hilly slopes of Meghalaya." Journal of Agrometeorology 8, no. 1 (2006): 81–86. http://dx.doi.org/10.54386/jam.v8i1.879.

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23

Sheng, Zhentao, Yaoyao Liao, Shuo Zhang, et al. "A Portable Pull-Out Soil Profile Moisture Sensor Based on High-Frequency Capacitance." Sensors 23, no. 8 (2023): 3806. http://dx.doi.org/10.3390/s23083806.

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Soil profile moisture is a crucial parameter of agricultural irrigation. To meet the demand of soil profile moisture, simple fast-sensing, and low-cost in situ detection, a portable pull-out soil profile moisture sensor was designed based on the principle of high-frequency capacitance. The sensor consists of a moisture-sensing probe and a data processing unit. The probe converts soil moisture into a frequency signal using an electromagnetic field. The data processing unit was designed for signal detection and transmitting moisture content data to a smartphone app. The data processing unit and

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24

An, Jing Qiang, Lin Rong Shi, and Feng Wei Zhang. "The Design of the Istallation Device for Soil Moisture Sensor." Advanced Materials Research 1049-1050 (October 2014): 1193–95. http://dx.doi.org/10.4028/www.scientific.net/amr.1049-1050.1193.

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For soil excavated a section is needed to dig in the direction of gravity artificial when soil moisture sensor is mounted against the general, and the size of cross section is proportional to the depth of buried sensors, making it time-consuming, and the original soil moisture distribution structure is destroyed, resulting in error between the original soil moisture and measured soil moisture profile is larger. A installation device for soil moisture sensor was designed in this paper, which can efficiently, rapidly, conveniently installation soil moisture sensors in the layered soil profile, a

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25

Kafarski, Marcin, Andrzej Wilczek, Agnieszka Szypłowska, et al. "Novel TDT Sensor for Soil Moisture Profile Probe." Proceedings 1, no. 8 (2017): 839. http://dx.doi.org/10.3390/proceedings1080839.

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Tužinský, L. "Soil moisture in mountain spruce stand." Journal of Forest Science 48, No. 1 (2019): 27–37. http://dx.doi.org/10.17221/11854-jfs.

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Mountain forests are among the main components of natural environment in Slovakia. They grow mainly in areas with cold climate, on poor soils with unfavorable reaction, often very acidic (pH in H<sub>2</sub>O &lt; 4.5) and with nutrient deficit. Immissions and acid rain attack forests to a great extent. Global climate changes also represent a new threat. Extremes in air temperatures, excessive amounts of precipitation or on the other hand the lack of water from precipitation, torrential rains or long-lasting drought periods are recorded as a result of a higher amount of heat en

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27

Yan, Guanxi, Thierry Bore, Zi Li, Stefan Schlaeger, Alexander Scheuermann, and Ling Li. "Application of Spatial Time Domain Reflectometry for Investigating Moisture Content Dynamics in Unsaturated Loamy Sand for Gravitational Drainage." Applied Sciences 11, no. 7 (2021): 2994. http://dx.doi.org/10.3390/app11072994.

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The strength of unsaturated soil is defined by the soil water retention behavior and soil suction acting inside the soil matrix. In order to obtain the suction and moisture profile in the vadose zone, specific measuring techniques are needed. Time domain reflectometry (TDR) conventionally measures moisture at individual points only. Therefore, spatial time domain reflectometry (spatial TDR) was developed for characterizing the moisture content profile along the unsaturated soil strata. This paper introduces an experimental set-up used for measuring dynamic moisture profiles with high spatial a

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Johnston, Benjamin R., William J. Randel, and Jeremiah P. Sjoberg. "Evaluation of Tropospheric Moisture Characteristics Among COSMIC-2, ERA5 and MERRA-2 in the Tropics and Subtropics." Remote Sensing 13, no. 5 (2021): 880. http://dx.doi.org/10.3390/rs13050880.

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Global navigation satellite system (GNSS) radio occultation (RO) receivers onboard the recently-launched COSMIC-2 (C2) satellite constellation provide an unprecedented number of high vertical resolution moisture profiles throughout the tropical and subtropical atmosphere. In this study, the distribution and variability of water vapor was investigated using specific humidity retrievals from C2 observations and compared to collocated ERA5 and MERRA-2 reanalysis profiles within 40°N to 40°S from September to December 2019, which is prior to the assimilation of C2 in the reanalyses. Negative C2 mo

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Le Morvan, Aurélie, Mehrez Zribi, Nicolas Baghdadi, and André Chanzy. "Soil Moisture Profile Effect on Radar Signal Measurement." Sensors 8, no. 1 (2008): 256–70. http://dx.doi.org/10.3390/s8010256.

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Vasilyev, S. M., V. N. Shkura, and A. S. Shtan'ko. "Local moisture zones profile of subdrip soil space." Agrarian Scientific Journal, no. 3 (March 18, 2019): 65–71. http://dx.doi.org/10.28983/asj.y2019i3pp65-71.

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Schlaeger, S. "A fast TDR-inversion technique for the reconstruction of spatial soil moisture content." Hydrology and Earth System Sciences Discussions 2, no. 3 (2005): 971–1009. http://dx.doi.org/10.5194/hessd-2-971-2005.

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Abstract. Spatial moisture distribution in natural soil or other material is a valuably information for many applications. Standard measurement techniques give only mean or pointwise results. Therefore a new inversion algorithm has been developed to derive moisture profiles along single TDR sensor-probes. The algorithm uses the full information content of TDR reflection data measured from one or both sides of an embedded probe. The system consisting of sensor probe and surrounded soil can be interpreted as a nonuniform transmission-line. The algorithm is based on the telegraph equations for no

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Collar, Concha. "Significance of heat-moisture treatment conditions on the pasting and gelling behaviour of various starch-rich cereal and pseudocereal flours." Food Science and Technology International 23, no. 7 (2017): 623–36. http://dx.doi.org/10.1177/1082013217714671.

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The impact of heat-moisture treatment processing conditions (15%, 25%, and 35% moisture content; 1, 3, and 5 h heating time at 120 ℃) on the viscosity pasting and gelling profiles of different grain flours matrices (barley, buckwheat, sorghum, high β-glucan barley, and wheat) was investigated by applying successive cooking and cooling cycles to rapid visco analyser canisters with highly hydrated samples (3.5:25, w:w). At a milder heat-moisture treatment conditions (15% moisture content, 1 h heating time), except for sorghum, heat-moisture treatment flours reached much higher viscosity values d

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Gribovszki, Zoltán. "Diurnal Method for Evapotranspiration Estimation from Soil Moisture Profile." Acta Silvatica et Lignaria Hungarica 10, no. 1 (2014): 67–75. http://dx.doi.org/10.2478/aslh-2014-0005.

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Abstract Water use of plants can be manifested in diurnal signal of soil moisture changes, and also of water table fluctuations in shallow water table environments. The signal can be especially strong in case of groundwater dependent forest vegetation with high water demand, where the water uptake is partly happening across the capillary zone. A new technique for water uptake estimation was elaborated on the basis of high frequency soil moisture profile data taking into account diurnally changing replenishment rate. The method is of great benefit to provide sufficient accuracy without soil spe

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Saad, Hasnida, Wan Muhammad Luqman Wan Ahmad Hilmi, Naimah Mat Isa, Noor Hafizah Abdul Aziz, and Lorena Ilagan. "Development of a Smart Profiling Sensor for Stingless Bee Honey Species in Malaysia." Journal of Advanced Research in Applied Sciences and Engineering Technology 64, no. 1 (2025): 95–109. https://doi.org/10.37934/araset.64.1.95109.

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The local stingless bee honey in Malaysia is highly valued because of its significant nutritional and natural remedy. Two commonly found stingless-bee species in Malaysia are Heterogona itama and Geniotrigona thoracica. Currently, the lack of standard profile data for the pure stingless bee honey from these two species leads to challenges in evaluating the authenticity of the stingless bee honey. To address this gap and provide a reliable solution, the objective of this research work is to develop a smart profiling system that can characterize stingless bee honey. This research work presents a

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Schlaeger, S. "A fast TDR-inversion technique for the reconstruction of spatial soil moisture content." Hydrology and Earth System Sciences 9, no. 5 (2005): 481–92. http://dx.doi.org/10.5194/hess-9-481-2005.

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Abstract. Spatial moisture distribution in natural soil or other material is a valuably information for many applications. Standard measurement techniques give only mean or punctual results. Therefore a new inversion algorithm has been developed to derive moisture profiles along single TDR sensor-probes. The algorithm uses the full information content of TDR reflection data measured from one or both sides of an embedded probe. The system consisting of sensor probe and surrounded soil can be interpreted as a nonuniform transmission-line. The algorithm is based on the telegraph equations for non

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36

Qin, Yan Fang, Ke Fa Zhou, Li Sun, Ming Jun Liu, and Qian Feng Wang. "Using GPR to Observe the Distribution of Soil Moisture and Reflector in Alpine Meadow of Urumqi Southern Mountain." Applied Mechanics and Materials 333-335 (July 2013): 219–25. http://dx.doi.org/10.4028/www.scientific.net/amm.333-335.219.

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Rapid determination of soil moisture in the arid area has important ecological significance and practical value. This study carried out a series of measurements in the alpine meadow of Urumqi Southern Mountain on April 28th, 2011 right after the snow melt. Ground-penetrating radar (GPR), time domain reflectometry (TDR) were used simultaneously for measuring the soil moisture of a 50 × 50 m2 plot, and a vertical soil profile was dug for validation analysis. The results show that: (1) a clear and continuous reflective layer in the experimental plot can be found from the GPR radar data and have a

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37

Scheffler, Gregor A., and Rudolf Plagge. "Application of instantaneous profile measurement of moisture content and moisture potential in porous materials." Materials and Structures 44, no. 8 (2011): 1517–36. http://dx.doi.org/10.1617/s11527-011-9716-y.

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Dewani, Noviana, Mirjana Sakradzija, Linda Schlemmer, Ronny Leinweber, and Juerg Schmidli. "Dependency of vertical velocity variance on meteorological conditions in the convective boundary layer." Atmospheric Chemistry and Physics 23, no. 7 (2023): 4045–58. http://dx.doi.org/10.5194/acp-23-4045-2023.

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Abstract. Measurements of vertical velocity from vertically pointing Doppler lidars are used to derive the profiles of normalized vertical velocity variance. Observations were taken during the FESSTVaL (Field Experiment on Submesoscale Spatio-Temporal Variability in Lindenberg) campaign during the warm seasons of 2020 and 2021. Normalized by the square of the convective velocity scale, the average vertical velocity variance profile follows the universal profile of Lenschow et al. (1980). However, daily profiles still show a high day-to-day variability. We found that moisture transport and the

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Saeed, Iftikhar Ahmed, Minjuan Wang, Yanzhao Ren, et al. "Performance analysis of dielectric soil moisture sensor." Soil and Water Research 14, No. 4 (2019): 195–99. http://dx.doi.org/10.17221/74/2018-swr.

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Soil moisture (SM) varies greatly in the soil profile. We developed a low-cost sensor for SM monitoring at three vertical depths. The sensor function was based on dielectric theory to monitor SM. Three linear calibration models were established using different soils. The sensor for each depth showed acceptable statistics of validations. The linear fit coefficient of determination (R<sup>2</sup>) ranged from 0.95 to 0.99. Root mean square error (RMSE) ranged from 1.35 to 4.30. The sensor performed consistently for at least 4 months, and is suitable for continuous monitoring of in si

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Chen, Xuelong, Yajing Liu, Yaoming Ma, et al. "TP-PROFILE: Monitoring the Thermodynamic Structure of the Troposphere over the Third Pole." Advances in Atmospheric Sciences 41, no. 6 (2024): 1264–77. http://dx.doi.org/10.1007/s00376-023-3199-y.

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AbstractGround-based microwave radiometers (MWRs) operating in the K- and V-bands (20–60 GHz) can help us obtain temperature and humidity profiles in the troposphere. Aside from some soundings from local meteorological observatories, the tropospheric atmosphere over the Tibetan Plateau (TP) has never been continuously observed. As part of the Chinese Second Tibetan Plateau Scientific Expedition and Research Program (STEP), the Tibetan Plateau Atmospheric Profile (TP-PROFILE) project aims to construct a comprehensive MWR troposphere observation network to study the synoptic processes and enviro

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Pengfei, Zhou, and Sergiy Ryzhkov. "RESEARCH OF SEPARATION GRADIENT AEROSOL TECHNOLOGIES FOR INTENSIFICATION OF HEAT AND MASS TRANSFER PROCESSES IN SYSTEMS OF HIGHLY TURBULENT DISPERSED BIPHASIC FLOWS. DEVELOPMENT OF SHIP SYSTEM FOR AIR FURIFICATION FROM DROPLET MOISTURE." Science Journal Innovation Technologies Transfer, no. 2019-2 (May 5, 2019): 70–85. http://dx.doi.org/10.36381/iamsti.2.2019.70-85.

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The study of gas dynamics and deposition coefficients of the separating profile has been performed. The three-dimensional model of working channels of the ship systems for air purification from droplet moisture is developed. The distribution of velocity, static pressure, dynamic pressure, kinetic energy of turbulence, and deposition coefficients for the flow rates of 5, 10, 15, 20 m/s in separating profiles with the radii of 5, 10, 15, 20, 25 mm. The droplet moisture deposition coefficient is 99.9 %. Designs of the ship systems for air purification from droplet moisture are developed for the a

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Mishra, Vikalp, James F. Cruise, Christopher R. Hain, John R. Mecikalski, and Martha C. Anderson. "Development of soil moisture profiles through coupled microwave–thermal infrared observations in the southeastern United States." Hydrology and Earth System Sciences 22, no. 9 (2018): 4935–57. http://dx.doi.org/10.5194/hess-22-4935-2018.

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Abstract. The principle of maximum entropy (POME) can be used to develop vertical soil moisture (SM) profiles. The minimal inputs required by the POME model make it an excellent choice for remote sensing applications. Two of the major input requirements of the POME model are the surface boundary condition and profile-mean moisture content. Microwave-based SM estimates from the Advanced Microwave Scanning Radiometer (AMSR-E) can supply the surface boundary condition whereas thermal infrared-based moisture estimated from the Atmospheric Land EXchange Inverse (ALEXI) surface energy balance model

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Kaneza, Nice, Aashish Pokhrel, Laureano R. Hoyos, and Xinbao Yu. "Thermally Induced Moisture Flow in a Silty Sand under a 1-D Thermal Gradient." Geosciences 14, no. 8 (2024): 207. http://dx.doi.org/10.3390/geosciences14080207.

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Thermally induced moisture flow in unsaturated soils involves complex coupled thermal–hydro processes with the moisture flow in both the vapor and liquid phases. The accurate measurement of the moisture flow in unsaturated sands remains a challenging task due to low moisture migration, the temperature effect on moisture sensors, and the gravity effect on moisture flow. This study aims to accurately measure transient moisture flow, heat transfer, and thermal conductivity in a silty sand with 35% non-plastic fines in a closed heat cell with a controlled 1-D temperature gradient. The heat cell co

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Nalli, Nicholas R., Christopher D. Barnet, Tony Reale, et al. "Satellite Sounder Observations of Contrasting Tropospheric Moisture Transport Regimes: Saharan Air Layers, Hadley Cells, and Atmospheric Rivers." Journal of Hydrometeorology 17, no. 12 (2016): 2997–3006. http://dx.doi.org/10.1175/jhm-d-16-0163.1.

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Abstract This paper examines the performance of satellite sounder atmospheric vertical moisture profiles under tropospheric conditions encompassing moisture contrasts driven by convection and advection transport mechanisms, specifically Atlantic Ocean Saharan air layers (SALs), tropical Hadley cells, and Pacific Ocean atmospheric rivers (ARs). Operational satellite sounder moisture profile retrievals from the Suomi National Polar-Orbiting Partnership (SNPP) NOAA Unique Combined Atmospheric Processing System (NUCAPS) are empirically assessed using collocated dedicated radiosonde observations (r

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Mostowik, Karolina, Agnieszka Kafel, Marta Kisiel, et al. "Zmienność temperatury i wilgotności gleby w pasmie Połoniny Wetlińskiej (Bieszczady Zachodnie)." Prace Geograficzne, no. 173 (February 2024): 57–85. http://dx.doi.org/10.4467/20833113pg.23.019.19231.

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The purpose of the research was to define the variability of soil temperature and moisture in three profiles in the Połonina Wetlińska Range in the period 23/11/2020–19/11/2021 and to assess the relationship between these parameters and meteorological conditions. Soil temperature and moisture loggers were situated at two depths (20 cm & 45 cm). Research has shown a higher soil temperature at a subsurface depth between the end of April and August. The soil temperature was strongly correlated with the air temperature in the warm half-year. The highest average soil temperature was observed fo

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Stankov, B. B., E. R. Westwater, and E. E. Gossard. "Use of Wind Profiler Estimates of Significant Moisture Gradients to Improve Humidity Profile Retrieval." Journal of Atmospheric and Oceanic Technology 13, no. 6 (1996): 1285–90. http://dx.doi.org/10.1175/1520-0426(1996)013<1285:uowpeo>2.0.co;2.

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Ansari, Sara, Neda Maftoon-Azad, Asgar Farahnaky, Ebrahim Hosseini, and Fojan Badii. "Effect of moisture content on textural attributes of dried figs." International Agrophysics 28, no. 4 (2014): 403–12. http://dx.doi.org/10.2478/intag-2014-0031.

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Abstract Due to their soft texture consumers prefer moist figs, which has motivated fig processors to increase the production of this product. However, as water enhances the browning reaction rate, moisture content optimisation of moist figs is very important. Processed figs must have suitable texture softness with browning kept to a minimum. The purpose of this study was to examine the effect of moisture content on the textural attributes of dried figs. Hardness, compression energy, gradient, gumminess and chewiness of fig samples decreased with moisture content exponentially, whereas the tre

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Phonetip, Khamtan, Graham Ian Brodie, Douangta Bouaphavong, Latsamy Boupha, and Somxay Khambouddaphan. "Drying Tectona grandis boards using the simulating solar kiln conditions technique." BioResources 15, no. 4 (2020): 9075–87. http://dx.doi.org/10.15376/biores.15.4.9075-9087.

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Timber cracking, drying stress residuals, and the change of moisture content profile were investigated during the drying of Tectona grandis boards in a conventional laboratory kiln. The study applied a technique that simulated solar kiln conditions using a conventional laboratory kiln to dry timber, based on Vientiane’s climatic conditions (Laos). The theoretical recharge and discharge model was used to generate the potential drying schedule for the Vientiane area; then the drying schedule was mimicked in a conventional laboratory kiln. Timber cracking and drying stress residual were monitored

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Fu, Xiao Lei, Zhong Bo Yu, Yu Li, et al. "One-Dimensional Soil Moisture Simulation Using Ensemble Kalman Filter." Applied Mechanics and Materials 212-213 (October 2012): 177–80. http://dx.doi.org/10.4028/www.scientific.net/amm.212-213.177.

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Data assimilation is a method which integrates model and observation. In hydrology, ensemble Kalman filter (EnKF) as a sequential data assimilation method is often used to correct model parameters, thus improve the simulated accuracy. In this study, we conduct one numerical experiment to predict soil moisture using the one-dimensional soil moisture system based on ensemble Kalman filter and Simple Biosphere (SiB2) Model at Meilin study area, China. The simulated period is divided into two parts: 0-60h and 60-240h. The results show that EnKF is an efficient method in assimilating the soil moist

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Rosolem, R., T. Hoar, A. Arellano, et al. "Assimilation of near-surface cosmic-ray neutrons improves summertime soil moisture profile estimates at three distinct biomes in the USA." Hydrology and Earth System Sciences Discussions 11, no. 5 (2014): 5515–58. http://dx.doi.org/10.5194/hessd-11-5515-2014.

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Abstract. Aboveground cosmic-ray neutron measurements provide an opportunity to infer soil moisture at the sub-kilometer scale. Initial efforts to assimilate those measurements have shown promise. This study expands such analysis by investigating (1) how the information from aboveground cosmic-ray neutrons can constrain the soil moisture at distinct depths simulated by a land surface model, and (2) how changes in data availability (in terms of retrieval frequency) impact the dynamics of simulated soil moisture profiles. We employ ensemble data assimilation techniques in a "nearly-identical twi

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