Evaporation.ppt
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This document discusses various processes of evaporation including evaporation, transpiration, and sublimation. It describes factors that influence evaporation such as energy supply, transport of vapor away from surfaces, and vegetated surfaces. Methods for estimating evaporation are discussed including the energy balance method, aerodynamic method, and combined method. The role of wind in enhancing evaporation and concepts of evapotranspiration from both soil and vegetation are also summarized.
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This document discusses various processes of evaporation and methods for estimating evaporation and evapotranspiration rates. It defines evaporation, transpiration, and sublimation and describes factors that influence evaporation like energy supply, transport of vapor, and vegetated surfaces. Methods for estimating evaporation rates include the energy balance method, aerodynamic method, and combined method. The document also provides an example calculation using the combined method.
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This document discusses various types of water losses from the landscape, including evaporation, evapotranspiration, and infiltration. It provides information on the processes, factors affecting them, and methods for measuring and estimating evaporation, evapotranspiration, and infiltration. Specifically, it describes evaporation pans and the process of pan evaporation, factors influencing evapotranspiration, and using a double ring infiltrometer to measure infiltration rates.
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diapositivas de introduccion a la hidrología y balance hidrológico
INTRODUCCION A LA HIDROLOGIA APLICADA
Solar radiation and evapotranspiration
Evaporation is a process by which water changed from the liquid or solid state into the gaseous state through the absorption of heat
It is always related to the loss of water from a free surface over a fixed time interval. Either direct observation or calculation based on the factors involved in the transfer of thermal energy.
One of the fundamental component of hydrological cycle
Essential requirements in the process are
The source of energy to vaporize the liquid water (solar or wind)
The presence of gradient of concentration between the evaporating surface and the surrounding air.
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EVAPORATION (LIQUID CONVERSION INTO VAPOUR PRESSURE)
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This document discusses various processes of evaporation and methods for estimating evaporation and evapotranspiration rates. It defines evaporation, transpiration, and sublimation and describes factors that influence evaporation like energy supply, transport of vapor, and vegetated surfaces. Methods for estimating evaporation rates include the energy balance method, aerodynamic method, and combined method. The document also provides an example calculation using the combined method.
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This document discusses various processes by which water changes phase from liquid to gas, including evaporation, transpiration, and sublimation. It provides details on the factors that control evaporation rates, such as energy inputs, temperature, humidity, wind, and water availability. It explains the differences between potential evapotranspiration (PET) and actual evapotranspiration (AET). Transpiration from plants and how it is affected by various environmental factors is also covered. Common methods for measuring and estimating evaporation and evapotranspiration are presented.
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This document discusses various types of water losses from the landscape, including evaporation, evapotranspiration, and infiltration. It provides information on the processes, factors affecting them, and methods for measuring and estimating evaporation, evapotranspiration, and infiltration. Specifically, it describes evaporation pans and the process of pan evaporation, factors influencing evapotranspiration, and using a double ring infiltrometer to measure infiltration rates.
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Most of Earth's water is found in oceans, which cover most of the planet's surface. The water cycle describes the continuous movement of water on, above, and below the Earth's surface, including evaporation, condensation, precipitation, and runoff. Evaporation occurs when water is heated by the sun and turns into water vapor, which rises up into the atmosphere and can form clouds and precipitation that falls back to Earth. [END SUMMARY]
diapositivas de introduccion a la hidrología y balance hidrológico
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Evaporation is a process by which water changed from the liquid or solid state into the gaseous state through the absorption of heat
It is always related to the loss of water from a free surface over a fixed time interval. Either direct observation or calculation based on the factors involved in the transfer of thermal energy.
One of the fundamental component of hydrological cycle
Essential requirements in the process are
The source of energy to vaporize the liquid water (solar or wind)
The presence of gradient of concentration between the evaporating surface and the surrounding air.
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The following file contains contents regarding Evaporation. Different methods to measure evaporations.
Primarily three methods are mentioned to measure Evaporation, that is Empirical Methods, Analytical Methods, and By using Evaporimeter or Pan.
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1. The document discusses various methods of measuring and estimating evaporation and transpiration from soil and plants. It describes the processes of interception, depression storage, evaporation and factors affecting evaporation.
2. Methods of measuring evaporation include pan observations using evaporation pans, atmospheric methods using atmometers, and empirical equations. Transpiration can be measured using a phytometer.
3. Evapotranspiration refers to the total water lost from an area due to evaporation from the soil and transpiration from plants. It is estimated using lysimeter methods, field experimental plots, or empirical equations like Blaney-Criddle.
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The document discusses various hydrological processes including interception, depression storage, infiltration, runoff, streamflow, and runoff modeling. It provides information on how interception by vegetation affects rainfall amounts and canopy storage capacity. Depression storage is explained as water trapped in low-lying areas that drains or infiltrates over time. Factors influencing infiltration rates and common measurement techniques are outlined. The generation of runoff from excess precipitation and factors controlling stream hydrographs are summarized. Finally, an overview of the development of conceptual runoff models and their applications is provided.
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Evaporation can be measured using lysimeters, which are devices that measure actual evapotranspiration from plants and soils. There are two main types of lysimeters - non-weighable lysimeters that measure percolation, and weighable lysimeters that directly measure weight changes. Weighable lysimeters can use mechanical scales, load cells, or hydraulic principles to continuously record the weight of the soil and calculate evapotranspiration from changes in water content over time. Lysimeters provide useful data for measuring actual evaporation and water budgets in agricultural and natural areas.
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This document discusses evapotranspiration, which is the total amount of water lost as vapor from soil, plant surfaces, and water bodies. It defines evaporation as movement of water to the air from sources like soil and water bodies, while transpiration is movement of water within plants and subsequent loss of water vapor through leaf stomata. The document outlines different types of evapotranspiration and factors that affect the process, like plant/crop characteristics, soil properties, and geographical factors. It also describes methods to determine evapotranspiration rates, including indirect methods like water balance and energy balance approaches, and direct methods like using lysimeters to measure actual evapotranspiration.
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Evaporation is the process where liquid water is converted to water vapor and moves from water and land surfaces into the atmosphere. Factors that influence the evaporation rate include temperature, humidity, wind speed, radiation, and vapor pressure difference between the air and water surface. Evaporation can be measured using evaporation pans, empirical equations, or analytical methods like water and energy budgeting. Reducing the surface area exposed, using wind breaks, or installing mechanical covers can help reduce evaporation from bodies of water.
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Evaporation is a key part of the water cycle that moves water around the planet. It is the process where liquid water transforms into water vapor due to energy, mainly from the sun. Several factors affect the evaporation rate, including temperature, humidity, wind speed, surface area, and salinity. Evaporation impacts cloud formation, water availability, climate regulation, and salinity balance. It can be measured directly using pans, lysimeters, and float gauges or indirectly through energy balance, water balance, and remote sensing methods.
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This document discusses evaporation and factors that influence it. It defines key terms like evaporation, transpiration, and sublimation. The main factors that influence evaporation are energy supply, transport of vapor away from the surface, and the moisture supply to vegetated surfaces. Methods for estimating evaporation rates include the energy balance method, aerodynamic method, and combined method. The document provides an example calculation of evaporation using the combined method. It also discusses evapotranspiration and potential evapotranspiration.
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The document defines key terms and concepts related to hydrology and the hydrological cycle. It describes water as moving through various stages of storage and transport within the drainage basin system, including precipitation, interception, evaporation, infiltration, soil moisture, groundwater, transpiration, and discharge. It notes that the hydrological cycle involves the movement of water between the atmosphere, lithosphere, and biosphere.
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Khilesh Kumar Sahu presented on factors determining water needs of crops. Evapotranspiration is the combined water loss from soil and plant surfaces through evaporation and transpiration. It is influenced by climatic factors like temperature, humidity, solar radiation and wind speed. Crop characteristics like crop type, leaf area, and root depth also impact water needs. Properly understanding evapotranspiration allows farmers to effectively schedule irrigation and maximize crop water utilization.
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The hydrologic cycle describes the constant circulation of water on Earth. Water evaporates from the oceans and atmosphere due to solar radiation. It exists as water vapor in the atmosphere and condenses to form clouds and precipitation. Precipitation falls back to Earth as rain, snow, or hail. Some precipitation is intercepted by vegetation or structures, where it either evaporates back into the atmosphere or flows across and through the ground as surface water or groundwater. Runoff water flows through streams and rivers back to the oceans, completing the cycle.
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This document discusses various concepts related to water resource engineering. It covers topics like precipitation, runoff, infiltration, evaporation and evapotranspiration. It describes different methods to measure these parameters, like using infiltration tests, pan evaporation, empirical equations and water or energy budget methods. Factors affecting each process are also listed. Various formulas to calculate runoff, evaporation and infiltration rate are presented.
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Estimation of evapotranspiration is important for improving water productivity. Evapotranspiration is the combination of evaporation from soil and transpiration from plants. Potential evapotranspiration is the maximum amount of water that can evaporate under optimal conditions, while actual evapotranspiration is lower due to environmental constraints. Lysimeters and models like Penman-Monteith can be used to measure and estimate evapotranspiration. Mulching and antitranspirants can help reduce evapotranspiration and improve water use efficiency of crops.
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The document discusses various methods for analyzing rainfall and runoff data in hydrology. It describes hyetographs and mass curves as ways to present rainfall intensity over time. Point rainfall data represents daily/weekly rainfall values in bar diagrams. Intensity-duration-frequency curves relate rainfall intensity, duration and probability. Depth-area-duration curves show the relationship between rainfall depth, area and duration. Infiltration and factors affecting it are also discussed. Common methods for measuring infiltration include single tube and double tube infiltrometers. Empirical equations, tables and regression models are presented for estimating runoff from rainfall-runoff data.
Evaporation
The following file contains contents regarding Evaporation. Different methods to measure evaporations.
Primarily three methods are mentioned to measure Evaporation, that is Empirical Methods, Analytical Methods, and By using Evaporimeter or Pan.
Abstractions of precipitation ppt
1. The document discusses various methods of measuring and estimating evaporation and transpiration from soil and plants. It describes the processes of interception, depression storage, evaporation and factors affecting evaporation.
2. Methods of measuring evaporation include pan observations using evaporation pans, atmospheric methods using atmometers, and empirical equations. Transpiration can be measured using a phytometer.
3. Evapotranspiration refers to the total water lost from an area due to evaporation from the soil and transpiration from plants. It is estimated using lysimeter methods, field experimental plots, or empirical equations like Blaney-Criddle.
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The document discusses various hydrological processes including interception, depression storage, infiltration, runoff, streamflow, and runoff modeling. It provides information on how interception by vegetation affects rainfall amounts and canopy storage capacity. Depression storage is explained as water trapped in low-lying areas that drains or infiltrates over time. Factors influencing infiltration rates and common measurement techniques are outlined. The generation of runoff from excess precipitation and factors controlling stream hydrographs are summarized. Finally, an overview of the development of conceptual runoff models and their applications is provided.
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Evaporation can be measured using lysimeters, which are devices that measure actual evapotranspiration from plants and soils. There are two main types of lysimeters - non-weighable lysimeters that measure percolation, and weighable lysimeters that directly measure weight changes. Weighable lysimeters can use mechanical scales, load cells, or hydraulic principles to continuously record the weight of the soil and calculate evapotranspiration from changes in water content over time. Lysimeters provide useful data for measuring actual evaporation and water budgets in agricultural and natural areas.
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This document discusses evaporation and evapotranspiration. It provides terminology for evaporation, transpiration, and evapotranspiration. Factors controlling evaporation include meteorological factors like solar radiation, relative humidity, temperature, and wind, as well as the nature of the evaporating surface. Methods to estimate evaporation include water budget, energy budget, mass transfer, combination methods, and evaporation formulas. Evaporation from free water surfaces can be estimated using these methods or evaporation pans with a pan coefficient. The document also discusses potential and actual evapotranspiration and methods to estimate them, including the Penman-Monteith equation and empirical methods.
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This document discusses evapotranspiration, which is the total amount of water lost as vapor from soil, plant surfaces, and water bodies. It defines evaporation as movement of water to the air from sources like soil and water bodies, while transpiration is movement of water within plants and subsequent loss of water vapor through leaf stomata. The document outlines different types of evapotranspiration and factors that affect the process, like plant/crop characteristics, soil properties, and geographical factors. It also describes methods to determine evapotranspiration rates, including indirect methods like water balance and energy balance approaches, and direct methods like using lysimeters to measure actual evapotranspiration.
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Evaporation is the process where liquid water is converted to water vapor and moves from water and land surfaces into the atmosphere. Factors that influence the evaporation rate include temperature, humidity, wind speed, radiation, and vapor pressure difference between the air and water surface. Evaporation can be measured using evaporation pans, empirical equations, or analytical methods like water and energy budgeting. Reducing the surface area exposed, using wind breaks, or installing mechanical covers can help reduce evaporation from bodies of water.
Evaporation: a key component of water cycle
Evaporation is a key part of the water cycle that moves water around the planet. It is the process where liquid water transforms into water vapor due to energy, mainly from the sun. Several factors affect the evaporation rate, including temperature, humidity, wind speed, surface area, and salinity. Evaporation impacts cloud formation, water availability, climate regulation, and salinity balance. It can be measured directly using pans, lysimeters, and float gauges or indirectly through energy balance, water balance, and remote sensing methods.
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Various instruments were used to measure environmental variables including a thermometer in a Stevenson screen, thermocouples connected to a data logger, a rain gauge, a rotating cup anemometer, a Kestrel 2500 hand-held weather meter, a sonic anemometer, a hygrometer, lux and light meters, and a Penman-Monteith equation requiring daily temperature, wind speed, humidity and solar radiation inputs to predict evapotranspiration. Additional instruments included a pyranometer, Campbell-Stoke Sunshine recorder, and Accupar to measure factors like solar radiation, sunshine, and photosynthetically active radiation.Evaporation (1).ppt
This document discusses evaporation and factors that influence it. It defines key terms like evaporation, transpiration, and sublimation. The main factors that influence evaporation are energy supply, transport of vapor away from the surface, and the moisture supply to vegetated surfaces. Methods for estimating evaporation rates include the energy balance method, aerodynamic method, and combined method. The document provides an example calculation of evaporation using the combined method. It also discusses evapotranspiration and potential evapotranspiration.
1.1 drainage basin system
The document defines key terms and concepts related to hydrology and the hydrological cycle. It describes water as moving through various stages of storage and transport within the drainage basin system, including precipitation, interception, evaporation, infiltration, soil moisture, groundwater, transpiration, and discharge. It notes that the hydrological cycle involves the movement of water between the atmosphere, lithosphere, and biosphere.
Soil, plant and meteorological factors determining water needs of crops
Khilesh Kumar Sahu presented on factors determining water needs of crops. Evapotranspiration is the combined water loss from soil and plant surfaces through evaporation and transpiration. It is influenced by climatic factors like temperature, humidity, solar radiation and wind speed. Crop characteristics like crop type, leaf area, and root depth also impact water needs. Properly understanding evapotranspiration allows farmers to effectively schedule irrigation and maximize crop water utilization.
Hydrologic cycle
The hydrologic cycle describes the constant circulation of water on Earth. Water evaporates from the oceans and atmosphere due to solar radiation. It exists as water vapor in the atmosphere and condenses to form clouds and precipitation. Precipitation falls back to Earth as rain, snow, or hail. Some precipitation is intercepted by vegetation or structures, where it either evaporates back into the atmosphere or flows across and through the ground as surface water or groundwater. Runoff water flows through streams and rivers back to the oceans, completing the cycle.
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Global warming is caused by greenhouse gases like carbon dioxide and methane that are released by human activities such as burning fossil fuels and deforestation. The average global temperature has already risen by 1°C in the past century and is projected to increase by over 1°C in the next 100 years if emissions continue rising. Some effects of climate change include rising sea levels from melting ice caps, more extreme weather, droughts, and loss of habitats. Individual actions like reducing waste, using less plastic, and buying locally grown food can help reduce greenhouse gas emissions and slow global warming.
ACID BASES AND SALTS.ppt
This document discusses acids, bases, and salts. It explains that acids contain hydrogen ions and bases contain hydroxide ions. When an acid and base react, they form water and a salt through a neutralization reaction. Salts are formed when hydrogen ions in an acid are replaced by metal ions. There are different types of salts including normal salts, acid salts, and basic salts depending on the reaction that forms them. Salts have various uses such as in fertilizers, drying agents, medicines, and gunpowder.
Solutions ppt.pptx
This document provides an overview of solutions and solubility. It defines key terms like solute, solvent, solution, homogeneous mixture, heterogeneous mixture, concentration, saturation, and factors that affect solubility. It also discusses quantitative concepts such as molarity, percent by mass, and how to use stoichiometry to calculate amounts in solutions. Specifically, it explains how to calculate amounts of solutes and solvents needed using molarity, percent by mass, and mole ratios from balanced chemical equations.
More from PapuKumarNaik1 (20)
Ch 14 short version directly from 14th New Edition saved 14 Feb 2012 and 15 A...
Ch 14 short version directly from 14th New Edition saved 14 Feb 2012 and 15 A...
Recently uploaded
原版制作(Manitoba毕业证书)曼尼托巴大学毕业证学位证一模一样
学校原件一模一样【微信：741003700 】《(Manitoba毕业证书)曼尼托巴大学毕业证学位证》【微信：741003700 】学位证，留信认证（真实可查，永久存档）原件一模一样纸张工艺/offer、雅思、外壳等材料/诚信可靠,可直接看成品样本，帮您解决无法毕业带来的各种难题！外壳，原版制作，诚信可靠，可直接看成品样本。行业标杆！精益求精，诚心合作，真诚制作！多年品质 ,按需精细制作，24小时接单,全套进口原装设备。十五年致力于帮助留学生解决难题，包您满意。
本公司拥有海外各大学样板无数，能完美还原。
1:1完美还原海外各大学毕业材料上的工艺：水印，阴影底纹，钢印LOGO烫金烫银，LOGO烫金烫银复合重叠。文字图案浮雕、激光镭射、紫外荧光、温感、复印防伪等防伪工艺。材料咨询办理、认证咨询办理请加学历顾问Q/微741003700
【主营项目】
一.毕业证【q微741003700】成绩单、使馆认证、教育部认证、雅思托福成绩单、学生卡等！
二.真实使馆公证(即留学回国人员证明,不成功不收费)
三.真实教育部学历学位认证（教育部存档！教育部留服网站永久可查）
四.办理各国各大学文凭(一对一专业服务,可全程监控跟踪进度)
如果您处于以下几种情况：
◇在校期间，因各种原因未能顺利毕业……拿不到官方毕业证【q/微741003700】
◇面对父母的压力，希望尽快拿到；
◇不清楚认证流程以及材料该如何准备；
◇回国时间很长，忘记办理；
◇回国马上就要找工作，办给用人单位看；
◇企事业单位必须要求办理的
◇需要报考公务员、购买免税车、落转户口
◇申请留学生创业基金
留信网认证的作用:
1:该专业认证可证明留学生真实身份
2:同时对留学生所学专业登记给予评定
3:国家专业人才认证中心颁发入库证书
4:这个认证书并且可以归档倒地方
5:凡事获得留信网入网的信息将会逐步更新到个人身份内，将在公安局网内查询个人身份证信息后，同步读取人才网入库信息
6:个人职称评审加20分
7:个人信誉贷款加10分
8:在国家人才网主办的国家网络招聘大会中纳入资料，供国家高端企业选择人才
Evolving Lifecycles with High Resolution Site Characterization (HRSC) and 3-D...
The incorporation of a 3DCSM and completion of HRSC provided a tool for enhanced, data-driven, decisions to support a change in remediation closure strategies. Currently, an approved pilot study has been obtained to shut-down the remediation systems (ISCO, P&T) and conduct a hydraulic study under non-pumping conditions. A separate micro-biological bench scale treatability study was competed that yielded positive results for an emerging innovative technology. As a result, a field pilot study has commenced with results expected in nine-twelve months. With the results of the hydraulic study, field pilot studies and an updated risk assessment leading site monitoring optimization cost lifecycle savings upwards of $15MM towards an alternatively evolved best available technology remediation closure strategy.
Optimizing Post Remediation Groundwater Performance with Enhanced Microbiolog...
Results of geophysics and pneumatic injection pilot tests during 2003 – 2007 yielded significant positive results for injection delivery design and contaminant mass treatment, resulting in permanent shut-down of an existing groundwater Pump & Treat system.
Accessible source areas were subsequently removed (2011) by soil excavation and treated with the placement of Emulsified Vegetable Oil EVO and zero-valent iron ZVI to accelerate treatment of impacted groundwater in overburden and weathered fractured bedrock. Post pilot test and post remediation groundwater monitoring has included analyses of CVOCs, organic fatty acids, dissolved gases and QuantArray® -Chlor to quantify key microorganisms (e.g., Dehalococcoides, Dehalobacter, etc.) and functional genes (e.g., vinyl chloride reductase, methane monooxygenase, etc.) to assess potential for reductive dechlorination and aerobic cometabolism of CVOCs.
In 2022, the first commercial application of MetaArray™ was performed at the site. MetaArray™ utilizes statistical analysis, such as principal component analysis and multivariate analysis to provide evidence that reductive dechlorination is active or even that it is slowing. This creates actionable data allowing users to save money by making important site management decisions earlier.
The results of the MetaArray™ analysis’ support vector machine (SVM) identified groundwater monitoring wells with a 80% confidence that were characterized as either Limited for Reductive Decholorination or had a High Reductive Reduction Dechlorination potential. The results of MetaArray™ will be used to further optimize the site’s post remediation monitoring program for monitored natural attenuation.
Kinetic studies on malachite green dye adsorption from aqueous solutions by A...
Kinetic studies on malachite green dye adsorption from aqueous solutions by A...Open Access Research Paper
Water polluted by dyestuffs compounds is a global threat to health and the environment; accordingly, we prepared a green novel sorbent chemical and Physical system from an algae, chitosan and chitosan nanoparticle and impregnated with algae with chitosan nanocomposite for the sorption of Malachite green dye from water. The algae with chitosan nanocomposite by a simple method and used as a recyclable and effective adsorbent for the removal of malachite green dye from aqueous solutions. Algae, chitosan, chitosan nanoparticle and algae with chitosan nanocomposite were characterized using different physicochemical methods. The functional groups and chemical compounds found in algae, chitosan, chitosan algae, chitosan nanoparticle, and chitosan nanoparticle with algae were identified using FTIR, SEM, and TGADTA/DTG techniques. The optimal adsorption conditions, different dosages, pH and Temperature the amount of algae with chitosan nanocomposite were determined. At optimized conditions and the batch equilibrium studies more than 99% of the dye was removed. The adsorption process data matched well kinetics showed that the reaction order for dye varied with pseudo-first order and pseudo-second order. Furthermore, the maximum adsorption capacity of the algae with chitosan nanocomposite toward malachite green dye reached as high as 15.5mg/g, respectively. Finally, multiple times reusing of algae with chitosan nanocomposite and removing dye from a real wastewater has made it a promising and attractive option for further practical applications.
RoHS stands for Restriction of Hazardous Substances, which is also known as t...
RoHS stands for Restriction of Hazardous Substances, which is also known as the Directive 2002/95/EC. It includes the restrictions for the use of certain hazardous substances in electrical and electronic equipment. RoHS is a WEEE (Waste of Electrical and Electronic Equipment).
Improving the viability of probiotics by encapsulation methods for developmen...
Improving the viability of probiotics by encapsulation methods for developmen...Open Access Research Paper
The popularity of functional foods among scientists and common people has been increasing day by day. Awareness and modernization make the consumer think better regarding food and nutrition. Now a day’s individual knows very well about the relation between food consumption and disease prevalence. Humans have a diversity of microbes in the gut that together form the gut microflora. Probiotics are the health-promoting live microbial cells improve host health through gut and brain connection and fighting against harmful bacteria. Bifidobacterium and Lactobacillus are the two bacterial genera which are considered to be probiotic. These good bacteria are facing challenges of viability. There are so many factors such as sensitivity to heat, pH, acidity, osmotic effect, mechanical shear, chemical components, freezing and storage time as well which affects the viability of probiotics in the dairy food matrix as well as in the gut. Multiple efforts have been done in the past and ongoing in present for these beneficial microbial population stability until their destination in the gut. One of a useful technique known as microencapsulation makes the probiotic effective in the diversified conditions and maintain these microbe’s community to the optimum level for achieving targeted benefits. Dairy products are found to be an ideal vehicle for probiotic incorporation. It has been seen that the encapsulated microbial cells show higher viability than the free cells in different processing and storage conditions as well as against bile salts in the gut. They make the food functional when incorporated, without affecting the product sensory characteristics.
Lessons from operationalizing integrated landscape approaches
Presented by James Reed at "9th Landscape Sustainability Science Forum" on 11 May 2024
快速办理(Calabria毕业证书)卡拉布里亚大学毕业证在读证明一模一样
原件一模一样【微信：bwp0011】《(Calabria毕业证书)卡拉布里亚大学毕业证》【微信：bwp0011】学位证，留信认证（真实可查，永久存档）原件一模一样纸张工艺/offer、雅思、外壳等材料/诚信可靠,可直接看成品样本，帮您解决无法毕业带来的各种难题！外壳，原版制作，诚信可靠，可直接看成品样本。行业标杆！精益求精，诚心合作，真诚制作！多年品质 ,按需精细制作，24小时接单,全套进口原装设备。十五年致力于帮助留学生解决难题，包您满意。
本公司拥有海外各大学样板无数，能完美还原。
1:1完美还原海外各大学毕业材料上的工艺：水印，阴影底纹，钢印LOGO烫金烫银，LOGO烫金烫银复合重叠。文字图案浮雕、激光镭射、紫外荧光、温感、复印防伪等防伪工艺。材料咨询办理、认证咨询办理请加学历顾问微bwp0011
【主营项目】
一.毕业证【微bwp0011】成绩单、使馆认证、教育部认证、雅思托福成绩单、学生卡等！
二.真实使馆公证(即留学回国人员证明,不成功不收费)
三.真实教育部学历学位认证（教育部存档！教育部留服网站永久可查）
四.办理各国各大学文凭(一对一专业服务,可全程监控跟踪进度)
如果您处于以下几种情况：
◇在校期间，因各种原因未能顺利毕业……拿不到官方毕业证【微bwp0011】
◇面对父母的压力，希望尽快拿到；
◇不清楚认证流程以及材料该如何准备；
◇回国时间很长，忘记办理；
◇回国马上就要找工作，办给用人单位看；
◇企事业单位必须要求办理的
◇需要报考公务员、购买免税车、落转户口
◇申请留学生创业基金
留信网认证的作用:
1:该专业认证可证明留学生真实身份
2:同时对留学生所学专业登记给予评定
3:国家专业人才认证中心颁发入库证书
4:这个认证书并且可以归档倒地方
5:凡事获得留信网入网的信息将会逐步更新到个人身份内，将在公安局网内查询个人身份证信息后，同步读取人才网入库信息
6:个人职称评审加20分
7:个人信誉贷款加10分
8:在国家人才网主办的国家网络招聘大会中纳入资料，供国家高端企业选择人才
在线办理(lboro毕业证书)拉夫堡大学毕业证学历证书一模一样
学校原件一模一样【微信：741003700 】《(lboro毕业证书)拉夫堡大学毕业证学历证书》【微信：741003700 】学位证，留信认证（真实可查，永久存档）原件一模一样纸张工艺/offer、雅思、外壳等材料/诚信可靠,可直接看成品样本，帮您解决无法毕业带来的各种难题！外壳，原版制作，诚信可靠，可直接看成品样本。行业标杆！精益求精，诚心合作，真诚制作！多年品质 ,按需精细制作，24小时接单,全套进口原装设备。十五年致力于帮助留学生解决难题，包您满意。
本公司拥有海外各大学样板无数，能完美还原。
1:1完美还原海外各大学毕业材料上的工艺：水印，阴影底纹，钢印LOGO烫金烫银，LOGO烫金烫银复合重叠。文字图案浮雕、激光镭射、紫外荧光、温感、复印防伪等防伪工艺。材料咨询办理、认证咨询办理请加学历顾问Q/微741003700
【主营项目】
一.毕业证【q微741003700】成绩单、使馆认证、教育部认证、雅思托福成绩单、学生卡等！
二.真实使馆公证(即留学回国人员证明,不成功不收费)
三.真实教育部学历学位认证（教育部存档！教育部留服网站永久可查）
四.办理各国各大学文凭(一对一专业服务,可全程监控跟踪进度)
如果您处于以下几种情况：
◇在校期间，因各种原因未能顺利毕业……拿不到官方毕业证【q/微741003700】
◇面对父母的压力，希望尽快拿到；
◇不清楚认证流程以及材料该如何准备；
◇回国时间很长，忘记办理；
◇回国马上就要找工作，办给用人单位看；
◇企事业单位必须要求办理的
◇需要报考公务员、购买免税车、落转户口
◇申请留学生创业基金
留信网认证的作用:
1:该专业认证可证明留学生真实身份
2:同时对留学生所学专业登记给予评定
3:国家专业人才认证中心颁发入库证书
4:这个认证书并且可以归档倒地方
5:凡事获得留信网入网的信息将会逐步更新到个人身份内，将在公安局网内查询个人身份证信息后，同步读取人才网入库信息
6:个人职称评审加20分
7:个人信誉贷款加10分
8:在国家人才网主办的国家网络招聘大会中纳入资料，供国家高端企业选择人才
Biomimicry in agriculture: Nature-Inspired Solutions for a Greener Future
Presentation made for the Webinar Series on Biomimicry for sustainability on 1st June 2024 organized by Green Building Council Sri Lanka
Environment Conservation Rules 2023 (ECR)-2023.pptx
Bangladesh Environment Conservation Rules 2023 (ECR-2023).
原版制作(Newcastle毕业证书)纽卡斯尔大学毕业证在读证明一模一样
学校原件一模一样【微信：741003700 】《(Newcastle毕业证书)纽卡斯尔大学毕业证》【微信：741003700 】学位证，留信认证（真实可查，永久存档）原件一模一样纸张工艺/offer、雅思、外壳等材料/诚信可靠,可直接看成品样本，帮您解决无法毕业带来的各种难题！外壳，原版制作，诚信可靠，可直接看成品样本。行业标杆！精益求精，诚心合作，真诚制作！多年品质 ,按需精细制作，24小时接单,全套进口原装设备。十五年致力于帮助留学生解决难题，包您满意。
本公司拥有海外各大学样板无数，能完美还原。
1:1完美还原海外各大学毕业材料上的工艺：水印，阴影底纹，钢印LOGO烫金烫银，LOGO烫金烫银复合重叠。文字图案浮雕、激光镭射、紫外荧光、温感、复印防伪等防伪工艺。材料咨询办理、认证咨询办理请加学历顾问Q/微741003700
【主营项目】
一.毕业证【q微741003700】成绩单、使馆认证、教育部认证、雅思托福成绩单、学生卡等！
二.真实使馆公证(即留学回国人员证明,不成功不收费)
三.真实教育部学历学位认证（教育部存档！教育部留服网站永久可查）
四.办理各国各大学文凭(一对一专业服务,可全程监控跟踪进度)
如果您处于以下几种情况：
◇在校期间，因各种原因未能顺利毕业……拿不到官方毕业证【q/微741003700】
◇面对父母的压力，希望尽快拿到；
◇不清楚认证流程以及材料该如何准备；
◇回国时间很长，忘记办理；
◇回国马上就要找工作，办给用人单位看；
◇企事业单位必须要求办理的
◇需要报考公务员、购买免税车、落转户口
◇申请留学生创业基金
留信网认证的作用:
1:该专业认证可证明留学生真实身份
2:同时对留学生所学专业登记给予评定
3:国家专业人才认证中心颁发入库证书
4:这个认证书并且可以归档倒地方
5:凡事获得留信网入网的信息将会逐步更新到个人身份内，将在公安局网内查询个人身份证信息后，同步读取人才网入库信息
6:个人职称评审加20分
7:个人信誉贷款加10分
8:在国家人才网主办的国家网络招聘大会中纳入资料，供国家高端企业选择人才
Wildlife-AnIntroduction.pdf so that you know more about our environment
All about wildlife, if you are fond of animals and wildlife then do follow us for more content like this
Recently uploaded (16)
world-environment-day-2024-240601103559-14f4c0b4.pptx
world-environment-day-2024-240601103559-14f4c0b4.pptx
Evolving Lifecycles with High Resolution Site Characterization (HRSC) and 3-D...
Evolving Lifecycles with High Resolution Site Characterization (HRSC) and 3-D...
BASIC CONCEPT OF ENVIRONMENT AND DIFFERENT CONSTITUTENET OF ENVIRONMENT
BASIC CONCEPT OF ENVIRONMENT AND DIFFERENT CONSTITUTENET OF ENVIRONMENT
Optimizing Post Remediation Groundwater Performance with Enhanced Microbiolog...
Optimizing Post Remediation Groundwater Performance with Enhanced Microbiolog...
Kinetic studies on malachite green dye adsorption from aqueous solutions by A...
Kinetic studies on malachite green dye adsorption from aqueous solutions by A...
RoHS stands for Restriction of Hazardous Substances, which is also known as t...
RoHS stands for Restriction of Hazardous Substances, which is also known as t...
Improving the viability of probiotics by encapsulation methods for developmen...
Improving the viability of probiotics by encapsulation methods for developmen...
Lessons from operationalizing integrated landscape approaches
Lessons from operationalizing integrated landscape approaches
Biomimicry in agriculture: Nature-Inspired Solutions for a Greener Future
Biomimicry in agriculture: Nature-Inspired Solutions for a Greener Future
Environment Conservation Rules 2023 (ECR)-2023.pptx
Environment Conservation Rules 2023 (ECR)-2023.pptx
Wildlife-AnIntroduction.pdf so that you know more about our environment
Wildlife-AnIntroduction.pdf so that you know more about our environment
Evaporation.ppt
- 1. Evaporation • Terminology – Evaporation – process by which liquid water passes directly to the vapor phase – Transpiration - process by which liquid water passes from liquid to vapor through plant metabolism – Sublimation - process by which water passes directly from the solid phase to the vapor phase
- 2. Factors Influencing Evaporation • Energy supply for vaporization (latent heat) – Solar radiation • Transport of vapor away from evaporative surface – Wind velocity over surface – Specific humidity gradient above surface • Vegetated surfaces – Supply of moisture to the surface – Evapotranspiration (ET) • Potential Evapotranspiration (PET) – moisture supply is not limited n R E Net radiation Evaporation Air Flow u
- 3. Evaporation from a Water Surface • Simplest form of evaporation – From free liquid of permanently saturated surface
- 4. Evaporation from a Pan • National Weather Service Class A type • Installed on a wooden platform in a grassy location • Filled with water to within 2.5 inches of the top • Evaporation rate is measured by manual readings or with an analog output evaporation gauge h Area, A CS w a AE m w v dt dh E n R s H Sensible heat to air Net radiation Vapor flow rate Heat conducted to ground G
- 5. Methods of Estimating Evaporation • Energy Balance Method • Aerodynamic method • Combined method
- 6. Wind as a Factor in Evaporation • Wind has a major effect on evaporation, E – Wind removes vapor-laden air by convection – This Keeps boundary layer thin – Maintains a high rate of water transfer from liquid to vapor phase – Wind is also turbulent • Convective diffusion is several orders of magnitude larger than molecular diffusion
- 7. Evapotranspiration • Evapotranspiration – Combination of evaporation from soil surface and transpiration from vegetation – Governing factors • Energy supply and vapor transport • Supply of moisture at evaporative surfaces – Reference crop • 8-15 cm of healthy growing green grass with abundant water – Combo Method works well if B is calibrated to local conditions