Relevant bibliographies by topics / Soil-plant-atmosphere

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Soil-plant-atmosphere'

Author: Grafiati
Published: 4 June 2021
Last updated: 8 February 2022

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Journal articles on the topic "Soil-plant-atmosphere"

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Haygarth, Philip M., Anthony F. Harrison, and Kevin C. Jones. "Plant Selenium from Soil and the Atmosphere." Journal of Environmental Quality 24, no. 4 (July 1995): 768–71. http://dx.doi.org/10.2134/jeq1995.00472425002400040030x.

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D. H. Fleisher, D. J. Timlin, Y. Yang, V. R. Reddy, and K. R. Reddy. "Uniformity of Soil-Plant-Atmosphere-Research Chambers." Transactions of the ASABE 52, no. 5 (2009): 1721–31. http://dx.doi.org/10.13031/2013.29134.

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Goldsmith, Gregory R. "Changing directions: the atmosphere-plant-soil continuum." New Phytologist 199, no. 1 (May 28, 2013): 4–6. http://dx.doi.org/10.1111/nph.12332.

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Werner, Christiane, and Maren Dubbert. "Resolving rapid dynamics of soil-plant-atmosphere interactions." New Phytologist 210, no. 3 (April 13, 2016): 767–69. http://dx.doi.org/10.1111/nph.13936.

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Baveye, Philippe C. "Review of Soil Physics with Python: Transport in the Soil-Plant-Atmosphere." Vadose Zone Journal 15, no. 3 (March 2016): vzj2015.12.0162br. http://dx.doi.org/10.2136/vzj2015.12.0162br.

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Boanares, Daniela, Rafael S. Oliveira, Rosy M. S. Isaias, Marcel G. C. França, and Josep Peñuelas. "The Neglected Reverse Water Pathway: Atmosphere–Plant–Soil Continuum." Trends in Plant Science 25, no. 11 (November 2020): 1073–75. http://dx.doi.org/10.1016/j.tplants.2020.07.012.

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I. A., Nweke,. "Potentials of Intercropping Systems to Soil - Water - Plant-Atmosphere." Agricultural Science 2, no. 1 (March 10, 2020): p31. http://dx.doi.org/10.30560/as.v2n1p31.

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A well planned intercropping system can efficiently serve as alternative to input such as fertilizer, herbicides, pesticides and pathogenicides. The interaction between the intercrop species, soil and environmental factors have positive effects on crop nutrition and photosynthesis and these have improved the nutrient content of the soil and different intercrop components. The high percentage ability of the intercrop species to suppress weeds especially when legume crops are involved in the plan, improves the physicochemical properties of the soil, contributes to the health of the intercrop species as the intercrop promotes the synthesis of allelopathic compounds and phenolic compounds such as anthocyanins and flavonoids which may serve as a deterrent to diseases and pests and improve the quality of the intercrop plants. Due to its inherent biological, biochemical and physiochemical properties intercropping system may be used to promote sustainable crop production and for safe management and cost-effective agricultural activities.
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Struik, P. C. "Modelling and parameterization of the soil-plant-atmosphere system." Potato Research 39, no. 1 (March 1996): 123–24. http://dx.doi.org/10.1007/bf02358211.

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Balashov, Eugene, Natalya Buchkina, Elena Rizhiya, and Csilla Farkas. "Field Validation of DNDC and SWAP Models for Temperature and Water Content of Loamy and Sandy Loam Spodosols." International Agrophysics 28, no. 2 (April 1, 2014): 133–42. http://dx.doi.org/10.2478/intag-2014-0001.

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Abstract The objectives of the research were to: fulfil the preliminary assessment of the sensitivity of the soil, water, atmosphere, and plant and denitrification and decomposition models to variations of climate variables based on the existing soil database; validate the soil, water, atmosphere, and plant and denitrification and decomposition modelled outcomes against measured records for soil temperature and water content. The statistical analyses were conducted by the sensitivity analysis, Nash-Sutcliffe efficiency coefficients and root mean square error using measured and modelled variables during three growing seasons. Results of sensitivity analysis demonstrated that: soil temperatures predicted by the soil, water, atmosphere, and plant model showed a more reliable sensitivity to the variations of input air temperatures; soil water content predicted by the denitrification and decomposition model had a better reliability in the sensitivity to daily precipitation changes. The root mean square errors and Nash-Sutcliffe efficiency coefficients demonstrated that: the soil, water, atmosphere, and plant model had a better efficiency in predicting seasonal dynamics of soil temperatures than the denitrification and decomposition model; and among two studied models, the denitrification and decomposition model showed a better capability in predicting the seasonal dynamics of soil water content.
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AODA, Tadao, and Shoji YOSHIDA. "Simulation model for soil water movement in soil-plant-atmosphere continuum considering hysteresis." Journal of Japan Society of Hydrology and Water Resources 8, no. 3 (1995): 322–34. http://dx.doi.org/10.3178/jjshwr.8.322.

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Dissertations / Theses on the topic "Soil-plant-atmosphere"

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Haygarth, Philip Matthew. "The role of the atmosphere in the cycling of selenium through soil-plant systems." Thesis, Lancaster University, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.284086.

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Wei, Jiangfeng. "Land-atmosphere interaction and climate variability." Diss., Available online, Georgia Institute of Technology, 2007, 2007. http://etd.gatech.edu/theses/available/etd-05162007-151312/.

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Thesis (Ph. D.)--Earth and Atmospheric Sciences, Georgia Institute of Technology, 2008.
Stieglitz, Marc, Committee Member ; Guillas, Serge, Committee Member ; Fu, Rong, Committee Member ; Curry, Judith, Committee Member ; Dickinson, Robert, Committee Chair.
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Manunta, Paolo. "Modelling strategies of the soil plant atmosphere continuum in water limited environments and elevated atmospheric CO¦2." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0010/NQ59998.pdf.

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Kuruppuarachchi, Don Stanley Premalal. "Productivity of irrigated potatoes in warm tropical lowlands influenced by water transport in the soil-plant-atmosphere continuum." Thesis, University of Reading, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.302821.

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Cheng, Li. "Elevated Atmospheric CO2 Impacts Carbon Dynamics in a C4-Sorghum-Soil Agroecosystem---An Application of Stable Carbon Isotopes (d13C) in Tracing the Fate of Carbon in the Atmosphere-Plant-Soil Ecosystem." Diss., Tucson, Arizona : University of Arizona, 2005. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu%5Fetd%5F1130%5F1%5Fm.pdf&type=application/pdf.

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Cavell, Julia, and Sara Andersson. "Long-term water modelling of the Soil-Plant-Atmosphere System : A study conducted for the growing of Grape Leaves with drip irrigation in the Binh Thuan Province, Vietnam." Thesis, KTH, Industriell ekologi, 2013. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-139384.

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The main objective was to set up models of the soil-plant-atmosphere system for the growing of Grape Leaves with drip irrigation in the Binh Thuan Province, Vietnam. The computer software tool CoupModel was used in this modelling process. The focus of the model was the systems soil hydraulics and the water balance between its components. When running several 21 years simulations it could be seen that slight variations in soil texture inputs resulted in relatively big output changes. For example, by either using the soil texture laboratory results or the soil water retention inputs gained from tensiometers and moisture meters in the field, gave an annual irrigation amount difference of 100 mm. However, it can be questioned if the models reached the goal of simulating an  efficient irrigation schedule  due to the soil evaporation output being high throughout the year.  For further research, longer time series of field measurements together with more knowledge about the plant would be preferable in order to validate and improve the model.
MÂlet med denna studie var att uppr‰tta modeller ˆver mark-v‰xt-atmosf‰r-systemet i programmet CoupModel. Modellerna skulle anpassas fˆr odlingen av vinblad med hj‰lp av droppbevattning i Binh Thuan-provinsen i Vietnam. Fokus i denna studie var vattenflˆden och vattenbalansen mellan systemets komponenter. Efter att ha kˆrt flera 21 Âr lÂnga simuleringar var det tydligt att sm variationer i indata resulterade i relativt stora skillnader i utdata. Om till exempel  v‰rden  angÂende jordartens struktur  erhÂllna  frÂn laboratoriet anv‰ndes ist‰llet fˆr f‰ltm‰tningar frÂn tensiometrar och fuktm‰tare blev det en Ârlig bevattningsskillnad p 100 mm. Det kan ifrÂgas‰ttas huruvida mÂlet att simulera en vatteneffektiv bevattning blev nÂtt d jordavdunstningen var hˆg Âret runt. Fˆr vidare studier skulle l‰ngre tidsserier av f‰ltm‰tningar tillsammans med mer kunskap om plantan vara nyttigt fˆr att kunna validera och fˆrb‰ttra modellen.
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Ribeiro, Rafael Vasconcelos. "Variação sazonal da fotossíntese e relações hídricas de laranjeira 'Valência'." Universidade de São Paulo, 2006. http://www.teses.usp.br/teses/disponiveis/11/11131/tde-23082006-152138/.

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Esse estudo tem como hipótese que a variação sazonal da fotossíntese de laranjeira ‘Valência’ está relacionada a fatores ambientais e endógenos. A menor atividade fotossintética durante os meses frios e secos está possivelmente associada à baixa temperatura e ao acúmulo de reservas, podendo ocorrer mesmo em condições de boa disponibilidade hídrica. A alta atividade fotossintética durante os meses quentes e chuvosos é possivelmente induzida pela maior disponibilidade de recursos naturais (água, energia solar e temperatura) e maior demanda por carboidratos, haja vista que nessa ocasião ocorre fluxo vegetativo intenso. O objetivo foi testar a hipótese acima, avaliando a variação anual de algumas características fisiológicas relacionadas à fotossíntese (trocas gasosas, fluorescência da clorofila, potencial de água no ramo e conteúdo foliar de carboidratos) de laranjeiras ‘Valência’ em condições de campo, em Cordeirópolis (SP). A influência da baixa disponibilidade hídrica sazonal foi verificada comparando-se plantas em condições naturais com plantas sob irrigação. A produção e algumas características biométricas foram avaliadas. A maior atividade fotossintética de laranjeiras ‘Valência’ ocorre durante a primavera, sendo induzida pelo aumento da temperatura e disponibilidade hídrica, enquanto que a menor fotossíntese ocorre durante o inverno, quando há baixa temperatura e deficiência hídrica. Durante o inverno, a menor fotossíntese não é associada ao conteúdo total de reservas foliares. Os valores máximos de assimilação de CO2 são observados na primavera, quando as condições ambientais são intermediárias entre o verão e o inverno e há fluxos vegetativo e reprodutivo nas laranjeiras. A alta demanda de carboidratos por esses drenos causa decréscimos no conteúdo de reservas foliares entre outubro e novembro, possivelmente estimulando a fotossíntese na primavera. Embora a fotossíntese das plantas no verão seja maior que no inverno, a atividade fotossintética não alcança valores próximos aos da primavera por limitações de origem bioquímica e estomática. A menor atividade bioquímica é induzida pela maior temperatura do ar em relação à primavera, em especial durante o período vespertino, enquanto que a limitação de origem estomática é causada pela alta demanda evaporativa do ar no verão. Durante o período quente e chuvoso, a atividade fotoquímica se ajusta às condições ambientais e não limita a fixação de carbono. A menor atividade fotossintética durante o inverno é ocasionada pela menor condutância estomática, devida à baixa temperatura do ar e solo. A ocorrência de deficiência hídrica no inverno causa redução do potencial de água nos ramos, diminuindo ainda mais a condutância estomática. No inverno, há limitação bioquímica da fotossíntese devida à baixa temperatura do ar, indicada pela redução da eficiência instantânea de carboxilação. Em relação ao metabolismo fotoquímico, não há indícios de limitação da fotossíntese.
This study has as hypothesis that the seasonal variation of photosynthesis in ‘Valencia’ sweet orange plant is related to environmental and endogenous factors. The lower photosynthetic activity during cold and dry months is possibly associated to low temperature and accumulation of leaf reserves, occurring even in well-watered plants.The higher photosynthetic activity during warm and rainy months is probably induced by higher availability of natural resources (water, sunlight and temperature) and by carbohydrate demand, since there is intense vegetative flush during this period. The objective was to test the above hyphotesis, evaluating the annual variation of some physiological characteristics related to photosynthesis (gas exchange, chlorophyll fluorescence, stem water potential and leaf carbohydrate content) of ‘Valencia’ sweet orange plants under field conditions, in Cordeirópolis (SP). The influence of low seasonal water availability was verified by comparing plants under natural with irrigated plants. Fruit production and some biometric characteristics were evaluated. The highest photosynthetic activity in ‘Valencia’ sweet orange plants occurred in spring, being induced by increase of temperature and water availability, while the lowest photosynthesis occurred in winter, when there is low temperature and water deficiency. During the winter, the lowest photosynthesis is not associated to the total reserve content in leaves. The maximum CO2 assimilation values are observed in spring, when environmental conditions are intermediate between summer and winter and there are vegetative and reproductive flushes in sweet orange plants. The high demand for carbohydrates in those sinks causes reduction in leaf reserve contents between october and november, probably estimulating the photosynthesis in spring. Although the photosynthesis in summer is higher than in winter, the photosynthetic activity does not reach values close to ones observed in spring due to biochemical and stomatal limitations. The low biochemical activity is induced by higher air temperature when compared to spring, mainly during afternoon, while the stomatal limitation is caused by the high air evaporative demand in summer. During the warm and wet period, the photochemical activity adjusts itself to environmental conditions and does not limit the carbon fixation. The low photosynthetic activity during winter is caused by low stomatal conductance as a consequence of low air and soil temperature. The occurrence of water deficiency in winter causes reduction of stem water potential, which is an additional factor leading to reduced stomatal conductance. In winter, there is biochemical limitation of photosynthesis due to low air temperature, as indicated by reduced instantaneous carboxylation efficiency. Regarding the photochemical metabolism, there are not signs of limitation to photosynthesis.
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Yetzer, Kenneth H. "Modeling the interaction between Plant Canopies and the Planetary Boundary Layer using a new 1D Multi-Layer Soil-Vegetation-Atmosphere Transfer (SVAT) Scheme combined with a Non-Local Turbulence Closure Model /." The Ohio State University, 1999. http://rave.ohiolink.edu/etdc/view?acc_num=osu148819327206972.

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Tang, Guoping. "An examination of vegetation modeling-related issues and the variation and climate sensitivity of vegetation and hydrology in China." Thesis, Connect to title online (Scholars' Bank) Connect to title online (ProQuest), 2008. http://hdl.handle.net/1794/8543.

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Thesis (Ph. D.)--University of Oregon, 2008.
Typescript. Includes vita and abstract. Includes bibliographical references (leaves 128-156). Also available online in Scholars' Bank; and in ProQuest, free to University of Oregon users.
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Medeiros, Almiro Tavares. "Estimativa da evapotranspiração de referência a partir da equação de Penman-Monteith, de medidas lisimétricas e de equações empíricas, em Paraipaba, CE." Universidade de São Paulo, 2002. http://www.teses.usp.br/teses/disponiveis/11/11143/tde-16072002-140154/.

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Tendo em vista a distribuição irregular de chuvas no nordeste, a irrigação se torna de grande importância, uma vez que passa a ser a principal alternativa racional de exploração das culturas agrícolas. Num projeto de irrigação, a evapotranspiração da cultura (ETc) é a variável mais importante, pois determina qual a quantidade de água a ser reposta, de forma a manter a produtividade a níveis rentáveis. Sendo a ETc função da evapotranspiração de referência (ETo), a determinação desta passa a ser fundamental em projetos, no planejamento e no manejo de irrigação. Dentro deste contexto o presente estudo teve por objetivo avaliar a estimativa da ETo, utilizando, para tanto, medidas lisimétricas e métodos de estimativa que foram comparados com valores de ETo obtidos com a equação de Penman-Monteith (Allen et al., 1998). Os métodos de estimativa de ETo empregados foram: Thornthwaite (1948), Thornthwaite modificado por Camargo et al. (1999), Tanque de Evaporação Classe A (Allen et al., 1998), Hargreaves & Samani (1985) e Priestley & Taylor (1972). A análise foi realizada em relação ao período de março a junho dos anos de 1997 e 1998, com dados coletados em uma estação meteorológica automática instalada na Estação Experimental do Vale do Curu, no Centro Nacional de Pesquisa em Agroindústria Tropical, pertencente à EMBRAPA, Paraipaba, CE, onde também se encontrava instalado um lisímetro de pesagem (área = 2,205m2), com células de carga. A análise foi baseada em dados diários, qüinqüidiais e decendiais, utilizando-se a análise de regressão, os índices de concordância de Willmott (1985) e de desempenho de Camargo e Sentelhas (1997), além dos seguintes erros: erro médio absoluto (EMA), erro máximo (EM), erro sistemático (Es) e erro aleatório (Ea). Os resultados obtidos mostraram que os dados medidos em lisímetro, se ajustaram de forma regular aos valores de ETo estimados pelo método de Penman-Monteith, nas três escalas de tempo avaliadas, o que indica a possibilidade de problemas na operação e manutenção desse dispositivo. Com relação aos métodos de estimativa de ETo, os que melhor se ajustaram aos valores obtidos por Penman-Monteith foram: Priestley & Taylor (1972) nas escalas diária e decendial e Thornthwaite modificado por Camargo et al. (1999) na escala qüinqüidial, porém, com erros sisitemáticos. Devido a isso, foram propostos ajustes com base nesses métodos. O ajuste constou de modificações no coeficiente ( f ) do método de Thornthwaite modificado por Camargo et al. (1999) e no parâmetro α da equação de Priestley-Taylor (1972), que foram modificados respectivamente para 0,379 e 1,19. Observou-se um desempenho considerado bom para o método de Priestley-Taylor (α = 1,19) e muito bom para Thornthwaite modificado por Camargo et al. (1999) (f = 0,379), indicando a potencialidade de seus usos em condições climáticas semelhantes às desse estudo, quando há limitação de dados meteorológicos.
The irregular distribuition of rain in the Brazil’s northeast region become irrigation very important, being the main rational alternative to produce food. In an irrigation project the crop evapotranspiration (ETc) is the most important variable, which determine how much water is necessary to be applied to maintain the yield at high levels. Being ETc funcion of reference evapotranspiration (ETo), the determination of this variabel is fundamental in irrigation projects and schedule. In this context, this study aimed to evaluate ETo estimates from lysimetric measures and other methods, which were compaired with the ETo values obtained by Penman-Monteith equation (Allen et al., 1998). The methods used were: Thornthwaite (1948), Thornthwaite modified by Camargo et al. (1999), Class A pan (Allen et al., 1998), Hargreaves & Samani (1985) and Priestley-Taylor (1972). The data were analysed during the period from march to june, in 1997 and 1998. The meteorological data were collected in an automatic weather station located at Vale do Curu Experimental Station, in the Tropical Agroindustry National Research Center, belonged to EMBRAPA, in Paraipaba, State of Ceará, Brazil, where a weighing lysimeter using strain gauge was installed (area = 2,205m2). The data analysis were based on daily, quinquidial and decendial time scale, and were done utilizing regression analysis, agreement (Willmott, 1981) and performance (Camargo & Sentelhas, 1997) indexes, and the following errors: absolute mean error (EMA), maximum error (EM), sistematic error (Es) and random error (Ea). The results obtained showed that ETo lysimeric measures did not fit well with ETo estimated by Penman-Monteith equation in all time scales evaluated, what problably is related to the problems in the operation and maintenance of this equipament. In relation to the other methods to estimate ETo, the best fits were obtained with Priestley-Taylor (1972), for daily and decendial data, and with Thornthwaite modified by Camargo et al. (1999), for quinquidial data. Howerer, these methods presented sistematic errors, being proposed adjusts in the parameters f for the Thornthwaite modified by Camargo et al. (1999) and α for the Priestley-Taylor methods, which were modified, recpectively, to 0.379 and 1.19. With these modifications these methods improved the ETo estimation, increasing the accuracy and decreasing the errors, being classified by the performance index as good and very good, indicating their potenciality for be used in similar climatic conditions of this study, where complete set of weather data are not available.
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Books on the topic "Soil-plant-atmosphere"

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Reichardt, Klaus, and Luís Carlos Timm. Soil, Plant and Atmosphere. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-19322-5.

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Novák, Viliam. Evapotranspiration in the Soil-Plant-Atmosphere System. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-3840-9.

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Novák, Viliam. Evapotranspiration in the Soil-Plant-Atmosphere System. Dordrecht: Springer Netherlands, 2012.

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Lindstrom, F. T. CTSPAC: Mathematical model for coupled transport of water, solutes, and heat in the soil-plant-atmosphere continuum. Corvallis, Or: Agricultural Experiment Station, Oregon State University, 1990.

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Cawlfield, David E. User's guide to CTSPAC: Mathematical model for coupled transport of water, solutes, and heat in the soil-plant-atmosphere continuum. Corvallis, OR: Agricultural Experiment Station, Oregon State University, 1990.

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Reichardt, Klaus, and Luís Carlos Timm. Soil, Plant and Atmosphere: Concepts, Processes and Applications. Springer, 2019.

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Soil Physics with Python: Transport in the Soil-Plant-Atmosphere System. Oxford University Press, 2015.

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Campbell, Gaylon S., Marco Bittelli, and Fausto Tomei. Soil Physics with Python: Transport in the Soil-Plant-Atmosphere System. Oxford University Press, 2020.

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Modelling and Parameterization of the Soil-Plant Atmosphere System. Purdue University Press, 2001.

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P, Kabat, ed. Modelling and parameterization of the soil-plant-atmosphere system: A comparison of potato growth models. Wageningen: Wageningen Pers, 1995.

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Book chapters on the topic "Soil-plant-atmosphere"

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Novák, Viliam. "Soil-Plant-Atmosphere System." In Evapotranspiration in the Soil-Plant-Atmosphere System, 15–24. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-3840-9_2.

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Sławiński, Cezary, and Henryk Sobczuk. "Soil–Plant–Atmosphere Continuum." In Encyclopedia of Agrophysics, 805–10. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-3585-1_141.

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Sutton, Julian. "Plant, Soil and Atmosphere." In Biology, 298–313. London: Macmillan Education UK, 1998. http://dx.doi.org/10.1007/978-1-349-15201-8_18.

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Reichardt, Klaus, and Luís Carlos Timm. "Man and the Soil–Plant–Atmosphere System." In Soil, Plant and Atmosphere, 1–6. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-19322-5_1.

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Reichardt, Klaus, and Luís Carlos Timm. "How Heat Is Propagated in the Soil." In Soil, Plant and Atmosphere, 209–15. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-19322-5_10.

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Reichardt, Klaus, and Luís Carlos Timm. "Water Infiltration into the Soil." In Soil, Plant and Atmosphere, 217–40. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-19322-5_11.

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Reichardt, Klaus, and Luís Carlos Timm. "Water Redistribution After Infiltration into the Soil." In Soil, Plant and Atmosphere, 241–57. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-19322-5_12.

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Reichardt, Klaus, and Luís Carlos Timm. "Evaporation and Evapotranspiration: The Vapor Losses to the Atmosphere." In Soil, Plant and Atmosphere, 259–73. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-19322-5_13.

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Reichardt, Klaus, and Luís Carlos Timm. "How Do Plants Absorb Soil Water?" In Soil, Plant and Atmosphere, 275–88. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-19322-5_14.

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Reichardt, Klaus, and Luís Carlos Timm. "The Water Balance in Agricultural and Natural Systems." In Soil, Plant and Atmosphere, 289–312. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-19322-5_15.

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Conference papers on the topic "Soil-plant-atmosphere"

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Trofymenko, P., N. Trofimenko, V. Zatserkovnyi, and F. Borysov. "Monitoring Of Emission Volumes ↔ Co2 Assimilation In «Soil-Atmosphere-Plant» System." In 12th International Conference on Monitoring of Geological Processes and Ecological Condition of the Environment. Netherlands: EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201803200.

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Draye, Xavier, and Lo Pag. "CrossTalk: A Simulation Platform for the Linking of Existing Soil, Plant and Atmosphere Models." In 2006 International Symposium on Plant Growth Modeling, Simulation, Visualization and Applications (PMA). IEEE, 2006. http://dx.doi.org/10.1109/pma.2006.49.

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Lobet, Guillaume, Loic Pages, and Xavier Draye. "A modeling approach to determine the contribution of plant hydraulic conductivities on the water uptake dynamics in the soil-plant-atmosphere system." In 2012 IEEE 4th International Symposium on Plant Growth Modeling, Simulation, Visualization and Applications (PMA). IEEE, 2012. http://dx.doi.org/10.1109/pma.2012.6524840.

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Guidi, V., B. Fabbri, M. Valt, S. Gherardi, A. Gaiardo, and C. Malagù. "P1AP.12 - Soil-Plant-Atmosphere System in Tomato and Maize Crops: Correlation of Gaseous Emissions to Water Stress." In 17th International Meeting on Chemical Sensors - IMCS 2018. AMA Service GmbH, Von-Münchhausen-Str. 49, 31515 Wunstorf, Germany, 2018. http://dx.doi.org/10.5162/imcs2018/p1ap.12.

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SASNAUSKIENĖ, Jurgita, Nomeda SABIENĖ, Vitas MAROZAS, Laima ČESONIENĖ, and Kristina LINGYTĖ. "SOIL RESPIRATION IN STANDS OF DIFFERENT TREE SPECIES." In RURAL DEVELOPMENT. Aleksandras Stulginskis University, 2018. http://dx.doi.org/10.15544/rd.2017.106.

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Forest ecosystems of different tree species participate actively in climatic and biotic processes, such as photosynthesis, plant and soil respiration, therefore knowledge of soil respiration, especially of CO2 emissions to the atmosphere is of great importance. The aim of the study was to determine soil respiration rate of stands of deciduous (Betula pubescens Ehrh., Quercus robur L.) and coniferous (Larix eurolepis Henry, Thuja occidentalis L.) tree species as well as impact of abiotic (soil temperature, humidity, electrical conductivity, pH) and biotic (abundance of undergrowth, shrub, herbs) factors. Measurements of CO2 emissions, temperature, moisture and electrical conductivity were performed in-situ in the stands of different tree species with portable ADC BioScientific LCpro+ system and digital electrochemical device “Wet” (Delta-T). Soil samples were collected for the physicochemical analysis simultaneously. Chemical analysis of soil samples was done at the lab of the Environmental Research of the Aleksandras Stulginskis University by standard methods. Soil respiration was highest in the stand of Thuja occidentalis and lowest in the stand of Betula pubescens. Soil respiration intensity of the tree stands increased as follow: Thuja˂ Quercus˂ Larix˂ Betula. In the coniferous tree stands, the soil respiration was lower on average 27% comparing to deciduous tree stands. Soil respiration rate increased with increase of herbaceous vegetation cover and temperature. Soil respiration rate was mostly influenced by abundance of herbaceous vegetation (r = 0.91) of all biotic factors investigated, while soil temperature (r = 0.75) of abiotic factors. 60 years old stands of different tree species formed specific conditions what influenced different soil respiration rates.
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Shurniak, Robert, Michael O’Kane, and Rosalind Green. "Simulation of seven years of field performance monitoring at Rio Tinto Iron Ore, Mount Tom Price Mine using soil-plant-atmosphere numerical modelling." In Seventh International Conference on Mine Closure. Australian Centre for Geomechanics, Perth, 2012. http://dx.doi.org/10.36487/acg_rep/1208_35_shurniak.

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Rudko, Georgii, and Maksym Ozerko. "ASSESSMENT OF ENVIRONMENTAL CHANGES DURING MINING OF FELDSPAR DEPOSITS IN UKRAINE." In GEOLINKS Conference Proceedings. Saima Consult Ltd, 2021. http://dx.doi.org/10.32008/geolinks2021/b1/v3/29.

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"Possible negative impacts on the environment during mining of feldspar deposits with open-pit and underground mine are defined. The main changes have been identified, which are as follows: air pollution, soil destructions, change of relief, a local decrease in groundwater level, pollution by sewage and waste. Destructions of the soil cover are fixed under the dumps of the quarry and in the path of the movement of quarry equipment. Through the development of a pit and dumps, the primary relief acquires significant changes and the action of forces caused primarily by gravity is activated, aimed at smoothing out negative and positive relief forms. An increase in the height difference from the dump ridge to the bottom of the quarry and the formation of a significant, pronounced depression of the relief redirects the surface runoff, increases its speed, and reduces infiltration into the soil. Mining development caused drainage of groundwater due to its release to the surface and evaporation. Air pollution has a bigger scale than other components of negative impacts. The main impact of mining activities is due to emissions of pollutants into the atmosphere as a result of blowing dust from the surface of dumps and emissions from quarry transport and their deposition on the soil and storage of industrial waste. The main pollutants are inorganic dust with content of SiO2 - 65-82% and Al2O3 - 11-21%. Separately, the article discusses the impact on the environment during multi-components deposits` exploitation, where feldspar concentrates are produced as by-products. Several deposits in Ukraine belong to the group: Bakhtyn (fluorite ores), Nosachivske (titanium-ilmenite ores), Perzhanske deposits of rare metals, Mazurivske (tantalum and niobium ores). Most of them are planned to be mined underground, which saves more land resources in comparison with open workings. The placement of mine shafts and industrial sites for their maintenance requires an area of about 30 hectares. All of them have a complex ore processing with the separation of several concentrates, which necessitates the use of flotation and other reagents. The development of such deposits involves the organization of tailings and circulating water supply of the processing plant."
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Yue, Ming, Linjing Zhang, Fengxue Gu, Xiaoling Pan, and Guifang Zhao. "The relationships between plant community species diversity and soil factors." In Third International Asia-Pacific Environmental Remote Sensing Remote Sensing of the Atmosphere, Ocean, Environment, and Space, edited by Xiaoling Pan, Wei Gao, Michael H. Glantz, and Yoshiaki Honda. SPIE, 2003. http://dx.doi.org/10.1117/12.466697.

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Shimada, Taro, Soichiro Ohshima, and Takenori Sukegawa. "Development of Safety Assessment Code for Decommissioning of Nuclear Facilities (DecDose)." In 17th International Conference on Nuclear Engineering. ASMEDC, 2009. http://dx.doi.org/10.1115/icone17-75123.

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A safety assessment code, DecDose, for decommissioning of nuclear facilities has been developed, based on the experiences of the decommissioning project of Japan Power Demonstration Reactor (JPDR) at Japan Atomic Energy Research Institute (now Japan Atomic Energy Agency). DecDose evaluates the annual exposure dose of the public and workers according to the progress of decommissioning of the plant, and also evaluates the public dose at accidental situations including fire and explosion. The public dose at normal situations during decommissioning is evaluated from the amount of radionuclides discharged from the plant to the atmosphere and the ocean. The amounts of radionuclides discharged depend on which and how activated and/or contaminated components and structures are dismantled. The amount is predicted by using the radioactive inventory given by the plant. The filtration efficiency of the ventilation system and decontamination factors of the liquid waste treatment system of the plant are also considered. Both of the internal dose caused by inhalation and ingestion of agricultural crops and seafood, and the external dose by radioactive aerosols airborne and radioactive deposition at soil surfaces are calculated for all of possible pathways. Also included in the external dose are direct radiation and skyshine radiation from waste containers which are packed and temporarily stored in the in-site building. For external dose of workers, the radiation dose rate from dismantling contaminated components and structures is calculated using the dose rate library which was previously evaluated by a point kernel shielding code. In this condition, radiation sources are regarded to be consisted of two parts; one is a dismantling object of interest, and the other is the sum of surrounding objects. Difference in job type or position is taken into account; workers for cutting are situated closer to a dismantling component, other workers help them at some distance, and the supervisor watches their activities from away. For worker’s internal dose, the radionuclide concentrations in air for individual radionuclides are calculated from a dismantling condition, e.g. cutting speed, cutting length of the dismantling component and exhaust velocity. A calculation model for working time on dismantling was developed using more segmented WBS (work breakdown structure). DecDose was partially verified by comparison with measured the external dose of workers during JPDR Decommissioning Project. The DecDose is expected to contribute to utilities in formulating rational dismantling plans and to the safety authority in estimating conservativeness in safety assessment of licensing application or risk-based regulatory criteria.
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Gu, Fengxue, Yu Chu, Yuandong Zhang, Yongqiang Liu, Subai Anabiek, Qian Ye, and Xiaoling Pan. "Spatial and temporal dynamics of soil moisture and salinity in typical plant communities of Sangonghe Basin." In Third International Asia-Pacific Environmental Remote Sensing Remote Sensing of the Atmosphere, Ocean, Environment, and Space, edited by Xiaoling Pan, Wei Gao, Michael H. Glantz, and Yoshiaki Honda. SPIE, 2003. http://dx.doi.org/10.1117/12.465997.

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Reports on the topic "Soil-plant-atmosphere"

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Renchon, Alexandre, Roser Matamala, Miquel Gonzalez-Meler, Zoe Cardon, Sébastien Lacube, Julie Jastrow, Beth Drewniak, Jules Cacho, and James Franke. Predictabilityand feedbacks of the ocean-soil-plant-atmosphere water cycle: deep learning water conductance in Earth System Model. Office of Scientific and Technical Information (OSTI), April 2021. http://dx.doi.org/10.2172/1769763.

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