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標(biāo)題: Titlebook: Evapotranspiration in the Soil-Plant-Atmosphere System; Viliam Novák Book 2012 Springer Science+Business Media Dordrecht. 2012 Evapotransp [打印本頁]

作者: INFER    時間: 2025-3-21 18:30
書目名稱Evapotranspiration in the Soil-Plant-Atmosphere System影響因子(影響力)




書目名稱Evapotranspiration in the Soil-Plant-Atmosphere System影響因子(影響力)學(xué)科排名




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書目名稱Evapotranspiration in the Soil-Plant-Atmosphere System網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Evapotranspiration in the Soil-Plant-Atmosphere System被引頻次




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書目名稱Evapotranspiration in the Soil-Plant-Atmosphere System讀者反饋




書目名稱Evapotranspiration in the Soil-Plant-Atmosphere System讀者反饋學(xué)科排名





作者: 厚顏    時間: 2025-3-21 21:45
Evapotranspiration in the Soil-Plant-Atmosphere System
作者: 寄生蟲    時間: 2025-3-22 03:00

作者: 傲慢物    時間: 2025-3-22 05:25

作者: GEST    時間: 2025-3-22 11:09
Evapotranspiration in the Soil-Plant-Atmosphere System978-94-007-3840-9Series ISSN 2352-4774 Series E-ISSN 2352-4782
作者: mortuary    時間: 2025-3-22 13:49

作者: mortuary    時間: 2025-3-22 18:47

作者: 潔凈    時間: 2025-3-23 01:14
,Ionic conductivities of Ch-Cl · glycerol,and energy cycles of the Earth. The physics of water phase change is briefly presented. Consumption of energy to change liquid water into water vapor cools the biosphere, thus allowing the creation of suitable conditions for life on the Earth. This chapter contains basic information about the Earth
作者: 引導(dǎo)    時間: 2025-3-23 01:30
Electrochemistry for a better environment,e biosphere is evapotranspiration. Evapotranspiration is, however, the process of water transport through the soil-plant-atmosphere system (SPAS). Every subsystem of the SPAS can strongly influence the evapotranspiration process. This chapter contains basic information about all three subsystems of
作者: adduction    時間: 2025-3-23 07:13
Reductive cyclizations at the cathode,eatures are accented. Evaporation of intercepted water, evaporation from water surfaces, from snow and ice as well as evaporation from urbanized surfaces is described. Transpiration as a process of water transport from soil through plant to the atmosphere is discussed. The basic features of water tr
作者: Resection    時間: 2025-3-23 09:49

作者: Innovative    時間: 2025-3-23 16:51

作者: 尊重    時間: 2025-3-23 21:22
Ceramics, Glasses, and Glazed Materials II,d solute) from the soil using the soil root layer. Evaporation is the typical movement of water to the soil surface (or close to it) from which water is evaporating. The properties of different plants’ root systems and their changes during ontogenesis is described, as well as the influence of differ
作者: peptic-ulcer    時間: 2025-3-23 23:05
Electrochemistry for Ecologistsion in the photosynthetic process is small in comparison with transpiration, which is enormous, and transpirating water passes through the plant and stomata to the atmosphere. To preserve itself, the plant can regulate transpiration by stomata opening and closing. Water movement through the plant is
作者: Ceramic    時間: 2025-3-24 02:39

作者: gangrene    時間: 2025-3-24 09:58

作者: Bouquet    時間: 2025-3-24 13:02
Joshua A. Hammons,Jan Ilavsky,Fan Zhangtion (from other surfaces). An approximative method of evapotranspiration structure calculation is presented. It is based on the empirically estimated relationship between the canopy leaf area index (LAI) and relative potential transpiration, i.e., on the ratio of potential transpiration and potenti
作者: 溫順    時間: 2025-3-24 18:31
Electrochemistry in Ionic Liquidsous evaporating surfaces. The method denoted as combination method is based in principle on the Penman-Monteith equation with modifications in calculation canopy resistance (using the Obuchov-Monin approach) and using empirical formulas to calculate evapotranspiration structure. Calculation is done
作者: 地名表    時間: 2025-3-24 21:46
Electrochemistry in Organic Synthesisanspiration. The weak point of traditional methods is the necessity to measure soil-plant-atmosphere system (SPAS) data at separate sites and upscale the information for regional evapotranspiration calculation. Many authors tried to use these data from the earliest days of the remote sensing techniq
作者: Harrowing    時間: 2025-3-25 00:14
https://doi.org/10.1007/978-94-007-3840-9Evapotranspiration; evaporation; soil hydrology; transpiration; water and energy transport; hydrogeology;
作者: 獨輪車    時間: 2025-3-25 04:18

作者: evince    時間: 2025-3-25 09:09

作者: Foreknowledge    時間: 2025-3-25 15:17
Evaporation from Different Surfaces,eatures are accented. Evaporation of intercepted water, evaporation from water surfaces, from snow and ice as well as evaporation from urbanized surfaces is described. Transpiration as a process of water transport from soil through plant to the atmosphere is discussed. The basic features of water tr
作者: 擦試不掉    時間: 2025-3-25 18:01

作者: 連鎖,連串    時間: 2025-3-25 22:58

作者: Indurate    時間: 2025-3-26 02:00

作者: Strength    時間: 2025-3-26 07:14

作者: 修飾    時間: 2025-3-26 10:31
Evapotranspiration and Soil Water,t of water to the evaporation surface or to the roots sometimes cannot cover potential evapotranspiration needs. The reason is the low hydraulic conductivity of the soil due to low soil water potential in the soil root zone. Then the evapotranspiration rate is less than the potential one, and the re
作者: Negligible    時間: 2025-3-26 15:28

作者: 協(xié)議    時間: 2025-3-26 19:30

作者: Factual    時間: 2025-3-26 20:59
Combination Method of Daily Evapotranspiration Calculation,ous evaporating surfaces. The method denoted as combination method is based in principle on the Penman-Monteith equation with modifications in calculation canopy resistance (using the Obuchov-Monin approach) and using empirical formulas to calculate evapotranspiration structure. Calculation is done
作者: 未開化    時間: 2025-3-27 04:18
Estimation of Regional Evapotranspiration Using Remote Sensing Data,anspiration. The weak point of traditional methods is the necessity to measure soil-plant-atmosphere system (SPAS) data at separate sites and upscale the information for regional evapotranspiration calculation. Many authors tried to use these data from the earliest days of the remote sensing techniq
作者: Statins    時間: 2025-3-27 05:31
2352-4774 water vapour transport between evaporating surface and atmo.Evapotranspiration and its components (evaporation and transpiration) as a process is one of the basic terms of? Earth‘s water balance; its importance is accented by the fact that transpiration is the vital element of the biomass productio
作者: 葡萄糖    時間: 2025-3-27 09:29

作者: Flinch    時間: 2025-3-27 14:48
,Ionic conductivities of Ch-Cl · glycerol,influencing evapotranspiration. The kinetic theory of evaporation can help us understand evaporation as a process, but does not allow use in directly quantifying it; therefore other methods should be used.
作者: 壯麗的去    時間: 2025-3-27 21:04
Patrik Schmuki,Sannakaisa Virtanened by transport coefficients. Methods of heat and water vapor transport coefficients estimation in the BLA are described. The influence of the state of an atmosphere on transport coefficients is discussed and the method of its quantification is given.
作者: EWE    時間: 2025-3-28 02:01

作者: 耕種    時間: 2025-3-28 05:56
Ceramics, Glasses, and Glazed Materials II,ake evaluation by roots, based on the results of field measurements. This method is used to model water movement and extraction by roots in soil with a plant canopy. The mesoscopic approach to water uptake by an evaluation of roots is described.
作者: harangue    時間: 2025-3-28 10:17
Electrochemistry for the Environmenton (evaporation) from potential data calculated using standard meteorological data. Using the relationship between relative transpiration (evaporation) to calculate actual data is preferred, because of easy evaluation of it in comparison with soil water potential.
作者: 某人    時間: 2025-3-28 12:44
Electrochemistry in Ionic Liquidsd meteorological data (air temperature, air humidity, sunshine duration, wind velocity), and soil root zone water content. Latitude of the site is needed to calculate net radiation. This chapter contains all the necessary tables needed to calculate daily rates of evapotranspiration; no other sources are needed.
作者: Shuttle    時間: 2025-3-28 17:30
Evapotranspiration: A Component of the Water Cycle,influencing evapotranspiration. The kinetic theory of evaporation can help us understand evaporation as a process, but does not allow use in directly quantifying it; therefore other methods should be used.
作者: 壓碎    時間: 2025-3-28 19:05
Transport of Water and Energy in the Boundary Layer of the Atmosphere,ed by transport coefficients. Methods of heat and water vapor transport coefficients estimation in the BLA are described. The influence of the state of an atmosphere on transport coefficients is discussed and the method of its quantification is given.
作者: insolence    時間: 2025-3-28 23:12
Movement of Water in Soil During Evaporation, in the field and in the laboratory are given, and the three stages of evaporation as they are related to the SWC are identified. A system of equations describing movement of liquid water, water vapor, and heat in the soil and approximative solution of transport equation for bare soil are presented.
作者: Graphite    時間: 2025-3-29 04:50

作者: chronology    時間: 2025-3-29 08:35
Evapotranspiration and Soil Water,on (evaporation) from potential data calculated using standard meteorological data. Using the relationship between relative transpiration (evaporation) to calculate actual data is preferred, because of easy evaluation of it in comparison with soil water potential.
作者: indignant    時間: 2025-3-29 13:33
Combination Method of Daily Evapotranspiration Calculation,d meteorological data (air temperature, air humidity, sunshine duration, wind velocity), and soil root zone water content. Latitude of the site is needed to calculate net radiation. This chapter contains all the necessary tables needed to calculate daily rates of evapotranspiration; no other sources are needed.
作者: Gum-Disease    時間: 2025-3-29 16:21

作者: ARIA    時間: 2025-3-29 21:26





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