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Journal articles on the topic 'Deposition-precipitation'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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1

Landau, M. V., L. Vradman, M. Herskowitz, Y. Koltypin, and A. Gedanken. "Ultrasonically Controlled Deposition–Precipitation." Journal of Catalysis 201, no. 1 (2001): 22–36. http://dx.doi.org/10.1006/jcat.2001.3227.

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2

Wei, M., A. J. Ruys, B. K. Milthorpe, and C. C. Sorrell. "Precipitation of hydroxyapatite nanoparticles: Effects of precipitation method on electrophoretic deposition." Journal of Materials Science: Materials in Medicine 16, no. 4 (2005): 319–24. http://dx.doi.org/10.1007/s10856-005-0630-0.

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3

Liechty, Hal O., Glenn D. Mroz, and David D. Reed. "Cation and anion fluxes in northern hardwood throughfall along an acidic deposition gradient." Canadian Journal of Forest Research 23, no. 3 (1993): 457–67. http://dx.doi.org/10.1139/x93-064.

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Ionic concentrations and fluxes were measured for 2 years in five northern hardwood stands along an acidic deposition gradient that extends from northern Minnesota (lowest deposition) to southeastern Michigan (highest deposition). Precipitation fluxes of H+, SO42−, and NO3− were, respectively, 340, 69, and 83% greater at the site with the highest deposition than at the site with the lowest deposition. No significant differences among sites were evident for precipitation fluxes of cations along the gradient. Fluxes of H+, SO42−, NO3−, Ca2+, and Mg2+ in throughfall increased along the gradient a

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4

Mohammed, Isah, Mohamed Mahmoud, Dhafer Al Shehri, Ammar El-Husseiny, and Olalekan Alade. "Asphaltene precipitation and deposition: A critical review." Journal of Petroleum Science and Engineering 197 (February 2021): 107956. http://dx.doi.org/10.1016/j.petrol.2020.107956.

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5

Weingarten, J. S., and J. A. Euchner. "Methods for Predicting Wax Precipitation and Deposition." SPE Production Engineering 3, no. 01 (1988): 121–26. http://dx.doi.org/10.2118/15654-pa.

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6

Souza, Kátia R., Adriana F. F. de Lima, Fernanda F. de Sousa, and Lucia Gorenstin Appel. "Preparing Au/ZnO by precipitation–deposition technique." Applied Catalysis A: General 340, no. 1 (2008): 133–39. http://dx.doi.org/10.1016/j.apcata.2008.02.006.

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7

Iavorivska, Lidiia, Elizabeth W. Boyer, and David R. DeWalle. "Atmospheric deposition of organic carbon via precipitation." Atmospheric Environment 146 (December 2016): 153–63. http://dx.doi.org/10.1016/j.atmosenv.2016.06.006.

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8

Cherednichenko, V. S., A. V. Cherednichenko, Al V. Cherednichenko, A. K. Zheksenbaeva, and A. S. Madibekov. "Heavy metal deposition through precipitation in Kazakhstan." Heliyon 7, no. 1 (2021): e05844. http://dx.doi.org/10.1016/j.heliyon.2020.e05844.

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9

Kimi, Melody, Bibie Nur Syafiqah Safiuddin, and Suh Cem Pang. "Catalytic Performance of Copper-Manganese Supported on Activated Carbon Synthesized by Deposition-Precipitation Method." Chemistry & Chemical Technology 14, no. 1 (2020): 32–37. http://dx.doi.org/10.23939/chcht14.01.032.

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10

Wałaszek, Kinga, Maciej Kryza, and Anthony J. Dore. "THE IMPACT OF PRECIPITATION ON WET DEPOSITION OF SULPHUR AND NITROGEN COMPOUNDS." Ecological Chemistry and Engineering S 20, no. 4 (2013): 733–45. http://dx.doi.org/10.2478/eces-2013-0051.

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Abstract Atmospheric transport model FRAME has been used in this study to estimate the influence of precipitation on the patterns of wet deposition of oxidised sulphur, oxidised nitrogen and reduced nitrogen in Poland during the years 1981-2005. A constant wind and emission data and year-specific spatially interpolated precipitation data was used in the model. The results show that the correlation coefficient between mean annual precipitation totals and mean wet deposition is above 0.9 for all examined compounds. The spatial patterns of pollutant deposition are similar for all years, with the

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11

Hong, Xiaowei, Ye Sun, Tianle Zhu, and Zhiming Liu. "Pt–Au/CeO2 catalysts for the simultaneous removal of carbon monoxide and formaldehyde." Catalysis Science & Technology 6, no. 10 (2016): 3606–15. http://dx.doi.org/10.1039/c5cy01744k.

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12

Jia, Meiqing, Zhiwei Gao, Huijun Gu, et al. "Effects of precipitation change and nitrogen addition on the composition, diversity, and molecular ecological network of soil bacterial communities in a desert steppe." PLOS ONE 16, no. 3 (2021): e0248194. http://dx.doi.org/10.1371/journal.pone.0248194.

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Currently, the impact of changes in precipitation and increased nitrogen(N) deposition on ecosystems has become a global problem. In this study, we conducted a 8-year field experiment to evaluate the effects of interaction between N deposition and precipitation change on soil bacterial communities in a desert steppe using high-throughput sequencing technology. The results revealed that soil bacterial communities were sensitive to precipitation addition but were highly tolerant to precipitation reduction. Reduced precipitation enhanced the competitive interactions of soil bacteria and made the

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13

Fu, Xuewu, Xu Yang, Xiaofang Lang, et al. "Atmospheric wet and litterfall mercury deposition at urban and rural sites in China." Atmospheric Chemistry and Physics 16, no. 18 (2016): 11547–62. http://dx.doi.org/10.5194/acp-16-11547-2016.

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Abstract. Mercury (Hg) concentrations and deposition fluxes in precipitation and litterfall were measured at multiple sites (six rural sites and an urban site) across a broad geographic area in China. The annual deposition fluxes of Hg in precipitation at rural sites and an urban site were 2.0 to 7.2 and 12.6 ± 6.5 µg m−2 yr−1, respectively. Wet deposition fluxes of Hg at rural sites showed a clear regional difference with elevated deposition fluxes in the subtropical zone, followed by the temporal zone and arid/semi-arid zone. Precipitation depth is the primary influencing factor causing the

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14

Cape, J. N., Y. S. Tang, J. González-Benítez, et al. "Organic nitrogen in precipitation across Europe." Biogeosciences Discussions 9, no. 7 (2012): 8093–109. http://dx.doi.org/10.5194/bgd-9-8093-2012.

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Abstract. Measurements of total nitrogen and inorganic nitrogen in precipitation samples from NitroEurope sites across Europe permit the calculation of organic nitrogen concentrations and wet deposition, by difference. The contribution of organic N to total N in precipitation ranged from only a few % to around 40% across sites from Northern Finland to Italy, similar to results from previous individual studies. This paper presents the absolute and relative contributions of organic N to wet N deposition across Europe, and examines seasonal trends. There were only weak correlations with other sol

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15

Cape, J. N., Y. S. Tang, J. M. González-Beníez, et al. "Organic nitrogen in precipitation across Europe." Biogeosciences 9, no. 11 (2012): 4401–9. http://dx.doi.org/10.5194/bg-9-4401-2012.

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Abstract. Measurements of total nitrogen and inorganic nitrogen in precipitation samples from NitroEurope sites across Europe permit the calculation of organic nitrogen concentrations and wet deposition, by difference. The contribution of organic N to total N in precipitation ranged from only a few % to around 40% across 18 sites from northern Finland to Italy, similar to results from previous individual studies. This paper presents the absolute and relative contributions of organic N to wet N deposition across Europe, and examines seasonal trends. There were only weak correlations with other

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16

Rong-tao, Li, Liao Xin-wei, Zou Jian-dong, et al. "Asphaltene Deposition during CO2 Flooding in Ultralow Permeability Reservoirs: A Case Study from Changqing Oil Field." Geofluids 2021 (June 3, 2021): 1–14. http://dx.doi.org/10.1155/2021/6626114.

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Asphaltene deposition is a common phenomenon during CO2 flooding in ultralow permeability reservoirs. The deposited asphaltene occupies the pore volume and decreases permeability, resulting in serious formation damage and pore well productivity. It is urgent to investigate the asphaltene deposition mechanisms, adverse effects, and preventive measures. However, few asphaltene deposition investigations have been systematically conducted by now. In this research, the asphaltene precipitation mechanisms and adverse effects were comprehensively investigated by using experimental and numerical metho

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17

Gerber, Franziska, Rebecca Mott, and Michael Lehning. "The Importance of Near-Surface Winter Precipitation Processes in Complex Alpine Terrain." Journal of Hydrometeorology 20, no. 2 (2019): 177–96. http://dx.doi.org/10.1175/jhm-d-18-0055.1.

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Abstract In this study, near-surface snow and graupel dynamics from formation to deposition are analyzed using WRF in a large-eddy configuration. The results reveal that a horizontal grid spacing of ≤50 m is required to resolve local orographic precipitation enhancement, leeside flow separation, and thereby preferential deposition. At this resolution, precipitation patterns across mountain ridges show a high temporal and spatial variability. Simulated and observed event-mean snow precipitation across three mountain ridges in the upper Dischma valley (Davos, Switzerland) for two precipitation e

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18

Tabzar, Amir, Mohammad Fathinasab, Afshin Salehi, Babak Bahrami, and Amir H. Mohammadi. "Multiphase flow modeling of asphaltene precipitation and deposition." Oil & Gas Science and Technology – Revue d’IFP Energies nouvelles 73 (2018): 51. http://dx.doi.org/10.2516/ogst/2018039.

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Asphaltene precipitation in reservoirs during production and Enhanced Oil Recovery (EOR) can cause serious problems that lead to reduction of reservoir fluid production. In order to study asphaltene tendency to precipitate and change in flow rate as a function of distance from wellbore, an equation of state (Peng-Robinson) based model namely Nghiem et al.’s model has been employed in this study. The heaviest components of crude oil are separated into two parts: The first portion is considered as non-precipitating component (C31A+) and the second one is considered as precipitating component (C3

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19

Nares, Rubén, Jorge Ramírez, Aída Gutiérrez-Alejandre, Catherine Louis та Tatiana Klimova. "Ni/Hβ-Zeolite Catalysts Prepared by Deposition−Precipitation". Journal of Physical Chemistry B 106, № 51 (2002): 13287–93. http://dx.doi.org/10.1021/jp0207679.

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20

Van Stiphout, P. C. M., A. J. Van Dillen, and J. W. Geus. "Electrochemically controlled deposition—precipitation of copper/silica catalysts." Applied Catalysis 37 (January 1988): 175–88. http://dx.doi.org/10.1016/s0166-9834(00)80759-9.

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21

Van Stiphout, P. C. M., C. R. Bayense, and J. W. Geus. "Electrochemically controlled deposition—precipitation of copper—nickel/silica." Applied Catalysis 37 (January 1988): 189–205. http://dx.doi.org/10.1016/s0166-9834(00)80760-5.

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22

Grimm, Jeffrey W., and James A. Lynch. "Enhanced Wet Deposition Estimates using Modeled Precipitation Inputs." Environmental Monitoring and Assessment 90, no. 1-3 (2004): 243–68. http://dx.doi.org/10.1023/b:emas.0000003592.56006.a0.

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23

Kühnel, Rafael, Tjarda J. Roberts, Mats P. Björkman, et al. "20-Year Climatology ofNO3 −andNH4 +Wet Deposition at Ny-Ålesund, Svalbard." Advances in Meteorology 2011 (2011): 1–10. http://dx.doi.org/10.1155/2011/406508.

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A 20-year dataset of weekly precipitation observations in Ny-Ålesund, Svalbard, was analysed to assess atmospheric wet deposition of nitrogen. Mean annual total nitrogen deposition was 74 mg N/(m2 yr) but exhibited large interannual variability and was dominated by highly episodic “strong” events, probably caused by rapid transport from European sources. The majority (90%) of precipitation samples were defined as “weak” (<2 mg N/m2) and contributed an annual baseline of ~17 mg N/(m2 yr), whereas 10% of precipitation samples were defined as “strong” (>2 mg N/m2) and additionally contribut

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24

Zapletal, Milos. "Atmospheric Deposition of Nitrogen and Sulphur Compounds in the Czech Republic." Scientific World JOURNAL 1 (2001): 294–303. http://dx.doi.org/10.1100/tsw.2001.88.

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Estimates of dry and wet deposition of nitrogen and sulphur compounds in the Czech Republic for the years 1994 and 1998 are presented. Deposition has been estimated from monitored and modeled concentrations in the atmosphere and in precipitation, where the most important acidifying compounds are sulphur diOxide, nitrogen Oxides, ammonia, and their reaction products. Measured atmospheric concentrations of SO2, NOx, NH3, and aerosol particles (SO42-, NO3–, and NH4+), along with measured concentrations of SO42-, NO3–, and NH4+in precipitation, weighted by precipitation amounts, were interpolated

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25

Groot Zwaaftink, C. D., A. Cagnati, A. Crepaz, et al. "Event-driven deposition: a new paradigm for snow-cover modelling in Antarctica based on surface measurements." Cryosphere Discussions 6, no. 5 (2012): 3575–612. http://dx.doi.org/10.5194/tcd-6-3575-2012.

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Abstract. Antarctic surface snow is studied by means of continuous measurements and observations over a period of 3 yr at Dome C. Snow observations include precipitation, daily records of deposition and erosion, snow temperatures at several depths, and snow profiles. Together with meteorological data from automatic weather stations, this forms a unique and complete dataset of snow conditions on the Antarctic Plateau. Large differences in snow amounts and density exist between precipitation measured 1 m above the surface and deposition on the surface. We then used the snow-cover model SNOWPACK

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26

Sprovieri, Francesca, Nicola Pirrone, Mariantonia Bencardino, et al. "Five-year records of mercury wet deposition flux at GMOS sites in the Northern and Southern hemispheres." Atmospheric Chemistry and Physics 17, no. 4 (2017): 2689–708. http://dx.doi.org/10.5194/acp-17-2689-2017.

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Abstract. The atmospheric deposition of mercury (Hg) occurs via several mechanisms, including dry and wet scavenging by precipitation events. In an effort to understand the atmospheric cycling and seasonal depositional characteristics of Hg, wet deposition samples were collected for approximately 5 years at 17 selected GMOS monitoring sites located in the Northern and Southern hemispheres in the framework of the Global Mercury Observation System (GMOS) project. Total mercury (THg) exhibited annual and seasonal patterns in Hg wet deposition samples. Interannual differences in total wet depositi

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27

Hole, L. R., H. A. de Wit, and W. Aas. "Influence of summer and winter climate variability on nitrogen wet deposition in Norway." Hydrology and Earth System Sciences 12, no. 2 (2008): 405–14. http://dx.doi.org/10.5194/hess-12-405-2008.

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Abstract. Dominating wind patterns around Norway may change due to climate warming. This could affect transport of polluted air masses and precipitation. Here, we study relations between reactive nitrogen wet deposition and air mass transport during summer and winter expressed in the form of climate indices, at seven sites in Southern Norway for the period 1980–2005. Atmospheric nitrate concentrations decreased with 0 to 50% in the period, particularly at sites with little precipitation, and mostly during 1990–2005. For comparison, reported reductions in emissions of oxidised nitrogen in Europ

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28

Hole, L. R., H. A. de Wit, and W. Aas. "Influence of summer and winter climate variability on nitrogen wet deposition in Norway." Hydrology and Earth System Sciences Discussions 4, no. 5 (2007): 3087–112. http://dx.doi.org/10.5194/hessd-4-3087-2007.

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Abstract. Dominating wind patterns around Norway may change due to climate warming. This could affect transport of polluted air masses and precipitation. Here, we study relations between reactive nitrogen wet deposition and air mass transport during summer and winter expressed in the form of climate indices, at seven sites in Southern Norway for the period 1980–2005. Atmospheric nitrate concentrations decreased with 0 to 50% in the period, particularly at sites with little precipitation, and mostly during 1990–2005. For comparison, reported reductions in emissions of oxidised nitrogen in Europ

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29

Rao, Leela E., John R. Matchett, Matthew L. Brooks, Robert F. Johnson, Richard A. Minnich, and Edith B. Allen. "Relationships between annual plant productivity, nitrogen deposition and fire size in low-elevation California desert scrub." International Journal of Wildland Fire 24, no. 1 (2015): 48. http://dx.doi.org/10.1071/wf13152.

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Although precipitation is correlated with fire size in desert ecosystems and is typically used as an indirect surrogate for fine fuel load, a direct link between fine fuel biomass and fire size has not been established. In addition, nitrogen (N) deposition can affect fire risk through its fertilisation effect on fine fuel production. In this study, we examine the relationships between fire size and precipitation, N deposition and biomass with emphasis on identifying biomass and N deposition thresholds associated with fire spreading across the landscape. We used a 28-year fire record of 582 bur

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30

Błaś, Marek, Katarzyna Cichała-Kamrowska, Mieczysław Sobik, Żaneta Polkowska, and Jacek Namieśnik. "Conditions controlling atmospheric pollutant deposition via snowpack." Environmental Reviews 18, NA (2010): 87–114. http://dx.doi.org/10.1139/a10-003.

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Solid precipitation represents a potentially important addition to other measures of deposition. However, an accurate estimate of snowfall amount and pollutant loading is not a trivial matter. There are obvious distinctions between regular precipitation collection and snowpack sampling that represent the cumulative chemistry of bulk deposition. The main goal is to show the most important processes and factors that may influence the rate and magnitude of pollutants deposition affected by the snowfall and snow cover: atmospheric pollutant enhancement of snowfall, pollutants deposition at snow co

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31

Dong, Ke, Cheolwoon Woo, and Naomichi Yamamoto. "Plant assemblages in atmospheric deposition." Atmospheric Chemistry and Physics 19, no. 18 (2019): 11969–83. http://dx.doi.org/10.5194/acp-19-11969-2019.

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Abstract. Plants disperse spores, pollen, and fragments into the atmosphere. The emitted plant particles return to the pedosphere by sedimentation (dry deposition) and/or by precipitation (wet deposition) and constitute part of the global cycle of substances. However, little is known regarding the taxonomic diversities and flux densities of plant particles deposited from the atmosphere. Here, plant assemblages were examined in atmospheric deposits collected in Seoul in South Korea. A custom-made automatic sampler was used to collect dry and wet deposition samples for which plant assemblages an

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32

Itahashi, Syuichi, Baozhu Ge, Keiichi Sato, et al. "Insights into seasonal variation of wet deposition over southeast Asia via precipitation adjustment from the findings of MICS-Asia III." Atmospheric Chemistry and Physics 21, no. 11 (2021): 8709–34. http://dx.doi.org/10.5194/acp-21-8709-2021.

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Abstract. Asia has attracted research attention because it has the highest anthropogenic emissions in the world, and the Model Inter-Comparison Study for Asia (MICS-Asia) phase III was carried out to foster our understanding of the status of air quality over Asia. This study analyzed wet deposition in southeast Asian countries (Myanmar, Thailand, Lao People's Democratic Republic (PDR), Cambodia, Vietnam, the Philippines, Malaysia, and Indonesia) with the aim of providing insights into the seasonal variation of wet deposition. Southeast Asia was not fully considered in MICS-Asia phase II due to

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33

Makowski Giannoni, S., R. Rollenbeck, K. Trachte, and J. Bendix. "Natural or anthropogenic? On the origin of atmospheric sulfate deposition in the Andes of southeastern Ecuador." Atmospheric Chemistry and Physics Discussions 14, no. 9 (2014): 13869–908. http://dx.doi.org/10.5194/acpd-14-13869-2014.

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Abstract. Atmospheric sulfur deposition above certain limits can represent a threat to tropical forests, causing nutrient imbalances and mobilizing toxic elements that impact biodiversity and forest productivity. Atmospheric sources of sulfur deposited by precipitation have being roughly identified in only a few lowland tropical forests. Even scarcer are these type of studies in tropical mountain forests, many of them megadiversity hotspots and especially vulnerable to acidic deposition. Here, the topographic complexity and related streamflow condition the origin, type, and intensity of deposi

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34

Makowski Giannoni, S., R. Rollenbeck, K. Trachte, and J. Bendix. "Natural or anthropogenic? On the origin of atmospheric sulfate deposition in the Andes of southeastern Ecuador." Atmospheric Chemistry and Physics 14, no. 20 (2014): 11297–312. http://dx.doi.org/10.5194/acp-14-11297-2014.

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Abstract. Atmospheric sulfur deposition above certain limits can represent a threat to tropical forests, causing nutrient imbalances and mobilizing toxic elements that impact biodiversity and forest productivity. Atmospheric sources of sulfur deposited by precipitation have been roughly identified in only a few lowland tropical forests. Even scarcer are studies of this type in tropical mountain forests, many of them mega-diversity hotspots and especially vulnerable to acidic deposition. In these places, the topographic complexity and related streamflow conditions affect the origin, type, and i

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35

Anseth, Ronnie, Nils-Olav Skeie, and Magne Waskaas. "The effect of precipitation and deposition layer growth on impedance measurements." tm - Technisches Messen 86, no. 1 (2019): 25–33. http://dx.doi.org/10.1515/teme-2018-0062.

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AbstractThe objective of the study was to examine how precipitation and deposition layer growth in an electrochemical cell impact impedance measurements. A measurement system, based on Electrochemical Impedance Spectroscopy (EIS), was used to observe the impedance of an electrochemical cell while precipitation was occurring. The measurement system was also used together with measurements of the solution concentration (in parts per million, ppm) to examine what impact deposition layer growth has on an electrochemical cell. Experimental results indicate a measurable change in the impedance magni

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36

Rastgoo, Abdolvahab, and Riyaz Kharrat. "Investigation of Asphaltene Deposition and Precipitation in Production Tubing." International Journal of Clean Coal and Energy 06, no. 01 (2017): 14–29. http://dx.doi.org/10.4236/ijcce.2017.61002.

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37

Krupa, S. V. "Acidic Precipitation. Volume 3: Sources, Deposition and Canopy Interactions." Journal of Environmental Quality 20, no. 3 (1991): 705. http://dx.doi.org/10.2134/jeq1991.00472425002000030040x.

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38

Kaulfus, Aaron S., Udaysankar Nair, Christopher D. Holmes, and William M. Landing. "Mercury Wet Scavenging and Deposition Differences by Precipitation Type." Environmental Science & Technology 51, no. 5 (2017): 2628–34. http://dx.doi.org/10.1021/acs.est.6b04187.

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39

Schaper, H., D. J. Amesz, E. B. M. Doesburg, P. H. M. de Korte, J. M. C. Quartel, and L. L. van Reijen. "Synthesis of thermostable nickel-alumina catalysts by deposition-precipitation." Applied Catalysis 16, no. 3 (1985): 417–29. http://dx.doi.org/10.1016/s0166-9834(00)84404-8.

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40

Burniston, Deborah A., William M. J. Strachan, and Robert J. Wilkinson. "Toxaphene Deposition to Lake Ontario via Precipitation, 1994−1998." Environmental Science & Technology 39, no. 18 (2005): 7005–11. http://dx.doi.org/10.1021/es050167y.

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41

Park, Soon-Ung, Hee-Jin In, and Young-Hee Lee. "Parameterization of wet deposition of sulfate by precipitation rate." Atmospheric Environment 33, no. 27 (1999): 4469–75. http://dx.doi.org/10.1016/s1352-2310(99)00200-9.

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42

Praus, Petr, Richard Dvorský, Petra Pustková, and Ondřej Kozák. "Precipitation of ZnS Nanoparticles and Their Deposition on Montmorillonite." Advanced Science, Engineering and Medicine 3, no. 1 (2011): 113–18. http://dx.doi.org/10.1166/asem.2011.1087.

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43

Dekker, Jan Pieter, Paul J. Van der Put, Hubert J. Veringa, and Joop Schoonman. "Particle-Precipitation-Aided Chemical Vapor Deposition of Titanium Nitride." Journal of the American Ceramic Society 80, no. 3 (1997): 629–36. http://dx.doi.org/10.1111/j.1151-2916.1997.tb02878.x.

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44

Rassamdana, Hossein, Bahram Dabir, Mehdi Nematy, Minoo Farhani, and Muhammad Sahimi. "Asphalt flocculation and deposition: I. The onset of precipitation." AIChE Journal 42, no. 1 (1996): 10–22. http://dx.doi.org/10.1002/aic.690420104.

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45

Barrie, L. A., and R. S. Schemenauer. "Pollutant wet deposition mechanisms in precipitation and fog water." Water, Air, and Soil Pollution 30, no. 1-2 (1986): 91–104. http://dx.doi.org/10.1007/bf00305178.

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46

Peretti, M., G. Piñeiro, M. E. Fernández Long, and D. A. Carnelos. "Influence of the precipitation interval on wet atmospheric deposition." Atmospheric Environment 237 (September 2020): 117580. http://dx.doi.org/10.1016/j.atmosenv.2020.117580.

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47

Narayanan, S., and G. Sreekanth. "Aromatic hydrogenation over nickel-silica prepared by deposition-precipitation." Reaction Kinetics & Catalysis Letters 51, no. 2 (1993): 449–58. http://dx.doi.org/10.1007/bf02069090.

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48

Bell, J. N. B. "Acidic precipitation. Volume 3: Sources, deposition and canopy interactions." Environmental Pollution 68, no. 1-2 (1990): 188–90. http://dx.doi.org/10.1016/0269-7491(90)90024-7.

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49

Iavorivska, Lidiia, Elizabeth W. Boyer, and David R. DeWalle. "Corrigendum to “Atmospheric deposition of organic carbon via precipitation”." Atmospheric Environment 262 (October 2021): 118565. http://dx.doi.org/10.1016/j.atmosenv.2021.118565.

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50

Semkin, R. G., and Dean S. Jeffries. "Bulk Deposition of Ions in the Turkey Lakes Watershed." Water Quality Research Journal 21, no. 4 (1986): 474–85. http://dx.doi.org/10.2166/wqrj.1986.041.

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Abstract Bulk deposition has been collected at the Turkey Lakes Watershed (near Sault Ste. Marie, Ontario) on a weekly basis since September 1981. Average precipitation quantity was 1212 mm over four years with rain fall accounting for approximately 70% of the total. The chemistry of bulk deposition is dominated by hydrogen and sulphate ions. Seasonal variations in chemistry were observed with summer concentrations of SO4, NH4, and Ca exceeding winter values by about 40%. The hydrogen ion content of hulk deposition is lower in the summer months while the SO4:NO3 equivalent ratio is at a maximu

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