Presentation given at the 2nd SILTFLUX workshop on 19/05/2015 at UCD. Authors: Elizabeth Conroy, Jonathan Turner, Michael Bruen, John O'Sullivan, Anna Rymszewicz, Mary Kelly-Quinn
Presentation given at the 2nd SILTFLUX workshop on 19/05/2015 at UCD. Authors: Michael Bruen, Mary Kelly-Quinn, John O'Sullivan, Jonathan Turner, Elizabeth Conroy, Anna Rymszewicz, Damian Lawler, John Wallace
In this 20-minute webinar, Dr. Colin Campbell demystifies the differences between soil water content measurement methods. He explores the scientific measurement theory and the pros and cons of each method. He also explains which technology might apply to different types of field research, and why modern sensing is about more than just the sensor.
Learn:
• Measurement theory behind the gravimetric method, capacitance, time-domain reflectometry (TDR), time-domain transmission (TDT), frequency-domain reflectometry (FDR), resistance sensors, and more
• Which technology applies to different field situations
• What factors matter when choosing a sensor type
• Why some methods are not research-grade
• How modern sensing is about more than just the sensor
• How to determine a good price-to-performance ratio for your unique application
Presentation given at the 2nd SILTFLUX workshop on 19/05/2015 at UCD. Authors: Elizabeth Conroy, Jonathan Turner, Michael Bruen, John O'Sullivan, Anna Rymszewicz, Mary Kelly-Quinn
Presentation given at the 2nd SILTFLUX workshop on 19/05/2015 at UCD. Authors: Michael Bruen, Mary Kelly-Quinn, John O'Sullivan, Jonathan Turner, Elizabeth Conroy, Anna Rymszewicz, Damian Lawler, John Wallace
In this 20-minute webinar, Dr. Colin Campbell demystifies the differences between soil water content measurement methods. He explores the scientific measurement theory and the pros and cons of each method. He also explains which technology might apply to different types of field research, and why modern sensing is about more than just the sensor.
Learn:
• Measurement theory behind the gravimetric method, capacitance, time-domain reflectometry (TDR), time-domain transmission (TDT), frequency-domain reflectometry (FDR), resistance sensors, and more
• Which technology applies to different field situations
• What factors matter when choosing a sensor type
• Why some methods are not research-grade
• How modern sensing is about more than just the sensor
• How to determine a good price-to-performance ratio for your unique application
Monitoring water pollution in the River Ganga with innovations in airborne remote sensing and drone technology.
Rajiv Sinha (Indian Institute of Technology Kanpur)
Editorial - May 2014 - Special Issue jointly coordinated by Mercator Ocean and Coriolis
focusing on Ocean Observations
Greetings all,
Once a year and for the fi fth year in a raw, the Mercator Ocean Forecasting Center in Toulouse and the Coriolis Infrastructure in Brest publish a
common newsletter. Some papers are dedicated to observations only, when others display collaborations between the 2 aspects: Observations and
Modelling/Data assimilation.
The fi rst paper by Cabanes et al. introducing this issue is presenting a new methodology aiming at correcting Argo fl oat salinity measurements in
delayed time when Argo fl oats conductivity sensors are subject to drift and offset due to bio-fouling or other technical problems.
Then, Cravatte et al. are using the Argo arrays in order to compile Argo fl oats’ drifts and show that they are a very valuable tool allowing determining
the absolute velocity. They apply this to study zonal jets at 1000 meters depth in the Tropics.
In the next paper, Maes and O’Kane provide with some results indicating the impact of a sustained ocean observing Argo network on the ability to
resolve the seasonal cycle of salinity stratifi cation by contrasting periods pre- and post-Argo. They take into account the respective thermal and saline
dependencies in the Brunt-Väisälä frequency (N2) in order to isolate the specifi c role of the salinity stratifi cation in the layers above the main pycno-
cline.
Picheral et al. are telling us about the Tara Oceans voyage that took place on the schooner “Tara” from 2009 to 2013 and visited all oceans. The ship
was adapted for modern oceanography. Scientifi c instruments were mounted on a dedicated CTD frame and installed on an underway fl ow-through
system. Data were sent daily to Coriolis. Post cruise calibrations were performed leading to a high quality dataset.
Then, Roquet et al. demonstrate the importance of the contribution of hydrographic and biogeochemical data collected by Antarctic marine mammals,
and in particular elephant seals, equipped with a new generation of oceanographic tags, for the environmental monitoring of the Southern Ocean.
The last paper of the present issue is displaying the collaboration between the Ocean Observations and Ocean Modelling communities: Turpin et
al. perform several Observing System Experiments in order to assess the impact of Argo observations on the Mercator Océan global analysis and
forecasting system at ¼ degree resolution.
We wish you a pleasant reading,
Laurence Crosnier and Sylvie Pouliquen, Editors.
#50
Newsletter
QUARTERLY
The Tara Oceans voyage took place on the schooner “Tara” from 2009 to 2013 and visited all oceans to collect samples and data in order to study the relationships between ecosystem biodiversity and function and the physical-chemical oceanographic environ-
ment (water mass, transport) (cf Picheral et al. this issue).
Credits: Francois Aurat/Tara Expéditions; Marc Picheral/LOV
Greetings all,
Once a year in April, the Mercator Ocean Forecasting Center in Toulouse and the Coriolis Infrastructure in Brest publish a common newsletter. Papers are dedicated to observations only.
• The first paper introducing this issue is presenting the Coriolis 2014-2020 framework which was renewed in 2014 in order to go on integrating in-situ ocean observation infrastructure for operational oceanography and ocean/climate research.
• Next paper by Poffa et al. describes how some Argo floats are deployed by the sailing community, through ship-based non-governmental organization or trans-oceanic races. It allows Argo floats to be deployed in poorly sampled areas where there is no regular shipping. Sailors got also involved in oceanographic science activities. An example of float deployment is given in the case of the Barcelona World Race.
• Next paper by Pouliquen et al. describes the EURO-ARGO ERIC infrastructure which is now officially set-up since May 2014. The objective of the Euro-Argo ERIC is to organize a long term European contribution to the international Argo array of profiling floats.
• Le Traon et al. are then presenting how the assessment of the impact of ARGO in Ocean models and satellite validation is conducted in the context of E-AIMS (Euro-Argo improvements for the GMES/Copernicus Marine Service) FP7 project. Observing System Evaluations and Observing System Simulation Experiments have been conducted to quantify the contribution of Argo to constrain global and regional monitoring and forecasting centers and validate satellite observations. Recommendations for the new phase of Argo are also elaborated.
• Kolodziejczyk et al. follow with the presentation of the complementarity of ARGO and SMOS Sea Surface Salinity (SSS) observations to help monitoring SSS variability from basin to meso scale. Using a 4-year time-series of SMOS SSS data and the global Argo array of in situ measurements, a statistical approach and an optimal interpolation method are used to characterize biases and reduce noises. Results are promising and show strong complementarity between SMOS and Argo data.
• Herbert et al. then describe Shipboard Acoustic Doppler Current Profilers (SADCP) observations which are carried out in the Tropical Atlantic during yearly cruises in the framework of the PIRATA program. The present note displays the SADCP data processing methodology applied for 8 PIRATA cruises by using CASCADE software.
• Cravatte et al. follow with a paper presenting the new international TPOS2020 project (2014-2020). The project objective is to build a renewed, integrated, internationally-coordinated and sustainable observing system in the Tropical Pacific, meeting both the needs of climate research and operational forecasting systems and learning lessons from the great success-and finally partial collapse- of the TAO/TRITON array.
• Saout-Grit et al. next present an updated procedure for CTD-oxygen calibration along with new
Commissioning of a 10 mld wwtp with flat sheet mbr technology the arenales de...WALEBUBLÉ
The authors are grateful to Professor Simon Judd & Claire Judd for the opportunity to publish this article on their renowned MBR-focused web page (www.thembrsite.com).
DEVELOPING THE OPTIMIZED OCEAN CURRENT STRENGTHENING DESALINATION SEMI-PERMEA...ijbesjournal
Alongside improvements in desalination operation and development of new technologies, problems of weakened counter current and global warming have emerged. Therefore, our study suggests a new desalination model, based on the experimental Support Vector Machine (SVM) algorithm, for semipermeable membrane separation. First, the reverse osmosis (RO) process used semi-permeable membrane and osmotic pressure to remove the solutes dissolved in seawater and obtain pure freshwater. The desalination process also applied MSF and MED, which are the best technologies developed through elimination of various problems that were previously experienced. This research is directed towards suggesting a model that can effectively create the semi-permeable membrane used in the desalination process. To efficiently prevent a counter current and safely obtain the water resources, an innovative technology is suggested by applying Genetic Algorithm (GA) to the SVM model for the semi-p
Conceptual Site Model Development and Environmental Molecular DiagnosticsAntea Group
This was presented at the 2019 Clemson Hydrogeology Symposium. Its full title is Conceptual Site Model Development and Environmental Molecular Diagnostics Use for PlumeStop(R) Liquid Activated Carbon(TM) Application at a Trichlorofluoromethane Groundwater Plume.
OMAE2013-10454: Experimental Study on Flow Around Circular Cylinders with Low...Rodolfo Gonçalves
Experiments were carried out in a recirculating water channel regarding the flow around stationary circular cylinders with low aspect ratio piercing the water free surface. Eight different aspect ratios were tested, namely L/D= 0.1, 0.2, 0.3, 0.5, 0.75, 1.0, 1.5 and 2.0; this range corresponds to aspect ratio related to circular offshore systems, such as spar and monocolumn platforms. Force was measured using a six degree-of-freedom load cell and Strouhal number is inferred through the transverse force fluctuation frequency. The range of Reynolds number covers 10,000 < Re < 50,000. PIV measurements were performed in some aspect ratio cases, namely 0.3, 0.5, 1.0 and 2.0 for Reynolds number equal to 43,000. The results showed a decrease in drag force coefficients with decreasing aspect ratio, as well as a decrease in Strouhal number with decreasing aspect ratio. The PIV showed the existence of an arch-type vortex originated in the cylinder free end.
New trends in earth sciences- Exploration of energy resourcesSwapnil Pal
A presentation on an article "strategies in geophysics: estimation of conventional and unconventional resources". Also a catchy analogy of a story "Nimboo pani" with role of a geologist in the current energy scenario.
Monitoring water pollution in the River Ganga with innovations in airborne remote sensing and drone technology.
Rajiv Sinha (Indian Institute of Technology Kanpur)
Editorial - May 2014 - Special Issue jointly coordinated by Mercator Ocean and Coriolis
focusing on Ocean Observations
Greetings all,
Once a year and for the fi fth year in a raw, the Mercator Ocean Forecasting Center in Toulouse and the Coriolis Infrastructure in Brest publish a
common newsletter. Some papers are dedicated to observations only, when others display collaborations between the 2 aspects: Observations and
Modelling/Data assimilation.
The fi rst paper by Cabanes et al. introducing this issue is presenting a new methodology aiming at correcting Argo fl oat salinity measurements in
delayed time when Argo fl oats conductivity sensors are subject to drift and offset due to bio-fouling or other technical problems.
Then, Cravatte et al. are using the Argo arrays in order to compile Argo fl oats’ drifts and show that they are a very valuable tool allowing determining
the absolute velocity. They apply this to study zonal jets at 1000 meters depth in the Tropics.
In the next paper, Maes and O’Kane provide with some results indicating the impact of a sustained ocean observing Argo network on the ability to
resolve the seasonal cycle of salinity stratifi cation by contrasting periods pre- and post-Argo. They take into account the respective thermal and saline
dependencies in the Brunt-Väisälä frequency (N2) in order to isolate the specifi c role of the salinity stratifi cation in the layers above the main pycno-
cline.
Picheral et al. are telling us about the Tara Oceans voyage that took place on the schooner “Tara” from 2009 to 2013 and visited all oceans. The ship
was adapted for modern oceanography. Scientifi c instruments were mounted on a dedicated CTD frame and installed on an underway fl ow-through
system. Data were sent daily to Coriolis. Post cruise calibrations were performed leading to a high quality dataset.
Then, Roquet et al. demonstrate the importance of the contribution of hydrographic and biogeochemical data collected by Antarctic marine mammals,
and in particular elephant seals, equipped with a new generation of oceanographic tags, for the environmental monitoring of the Southern Ocean.
The last paper of the present issue is displaying the collaboration between the Ocean Observations and Ocean Modelling communities: Turpin et
al. perform several Observing System Experiments in order to assess the impact of Argo observations on the Mercator Océan global analysis and
forecasting system at ¼ degree resolution.
We wish you a pleasant reading,
Laurence Crosnier and Sylvie Pouliquen, Editors.
#50
Newsletter
QUARTERLY
The Tara Oceans voyage took place on the schooner “Tara” from 2009 to 2013 and visited all oceans to collect samples and data in order to study the relationships between ecosystem biodiversity and function and the physical-chemical oceanographic environ-
ment (water mass, transport) (cf Picheral et al. this issue).
Credits: Francois Aurat/Tara Expéditions; Marc Picheral/LOV
Greetings all,
Once a year in April, the Mercator Ocean Forecasting Center in Toulouse and the Coriolis Infrastructure in Brest publish a common newsletter. Papers are dedicated to observations only.
• The first paper introducing this issue is presenting the Coriolis 2014-2020 framework which was renewed in 2014 in order to go on integrating in-situ ocean observation infrastructure for operational oceanography and ocean/climate research.
• Next paper by Poffa et al. describes how some Argo floats are deployed by the sailing community, through ship-based non-governmental organization or trans-oceanic races. It allows Argo floats to be deployed in poorly sampled areas where there is no regular shipping. Sailors got also involved in oceanographic science activities. An example of float deployment is given in the case of the Barcelona World Race.
• Next paper by Pouliquen et al. describes the EURO-ARGO ERIC infrastructure which is now officially set-up since May 2014. The objective of the Euro-Argo ERIC is to organize a long term European contribution to the international Argo array of profiling floats.
• Le Traon et al. are then presenting how the assessment of the impact of ARGO in Ocean models and satellite validation is conducted in the context of E-AIMS (Euro-Argo improvements for the GMES/Copernicus Marine Service) FP7 project. Observing System Evaluations and Observing System Simulation Experiments have been conducted to quantify the contribution of Argo to constrain global and regional monitoring and forecasting centers and validate satellite observations. Recommendations for the new phase of Argo are also elaborated.
• Kolodziejczyk et al. follow with the presentation of the complementarity of ARGO and SMOS Sea Surface Salinity (SSS) observations to help monitoring SSS variability from basin to meso scale. Using a 4-year time-series of SMOS SSS data and the global Argo array of in situ measurements, a statistical approach and an optimal interpolation method are used to characterize biases and reduce noises. Results are promising and show strong complementarity between SMOS and Argo data.
• Herbert et al. then describe Shipboard Acoustic Doppler Current Profilers (SADCP) observations which are carried out in the Tropical Atlantic during yearly cruises in the framework of the PIRATA program. The present note displays the SADCP data processing methodology applied for 8 PIRATA cruises by using CASCADE software.
• Cravatte et al. follow with a paper presenting the new international TPOS2020 project (2014-2020). The project objective is to build a renewed, integrated, internationally-coordinated and sustainable observing system in the Tropical Pacific, meeting both the needs of climate research and operational forecasting systems and learning lessons from the great success-and finally partial collapse- of the TAO/TRITON array.
• Saout-Grit et al. next present an updated procedure for CTD-oxygen calibration along with new
Commissioning of a 10 mld wwtp with flat sheet mbr technology the arenales de...WALEBUBLÉ
The authors are grateful to Professor Simon Judd & Claire Judd for the opportunity to publish this article on their renowned MBR-focused web page (www.thembrsite.com).
DEVELOPING THE OPTIMIZED OCEAN CURRENT STRENGTHENING DESALINATION SEMI-PERMEA...ijbesjournal
Alongside improvements in desalination operation and development of new technologies, problems of weakened counter current and global warming have emerged. Therefore, our study suggests a new desalination model, based on the experimental Support Vector Machine (SVM) algorithm, for semipermeable membrane separation. First, the reverse osmosis (RO) process used semi-permeable membrane and osmotic pressure to remove the solutes dissolved in seawater and obtain pure freshwater. The desalination process also applied MSF and MED, which are the best technologies developed through elimination of various problems that were previously experienced. This research is directed towards suggesting a model that can effectively create the semi-permeable membrane used in the desalination process. To efficiently prevent a counter current and safely obtain the water resources, an innovative technology is suggested by applying Genetic Algorithm (GA) to the SVM model for the semi-p
Conceptual Site Model Development and Environmental Molecular DiagnosticsAntea Group
This was presented at the 2019 Clemson Hydrogeology Symposium. Its full title is Conceptual Site Model Development and Environmental Molecular Diagnostics Use for PlumeStop(R) Liquid Activated Carbon(TM) Application at a Trichlorofluoromethane Groundwater Plume.
OMAE2013-10454: Experimental Study on Flow Around Circular Cylinders with Low...Rodolfo Gonçalves
Experiments were carried out in a recirculating water channel regarding the flow around stationary circular cylinders with low aspect ratio piercing the water free surface. Eight different aspect ratios were tested, namely L/D= 0.1, 0.2, 0.3, 0.5, 0.75, 1.0, 1.5 and 2.0; this range corresponds to aspect ratio related to circular offshore systems, such as spar and monocolumn platforms. Force was measured using a six degree-of-freedom load cell and Strouhal number is inferred through the transverse force fluctuation frequency. The range of Reynolds number covers 10,000 < Re < 50,000. PIV measurements were performed in some aspect ratio cases, namely 0.3, 0.5, 1.0 and 2.0 for Reynolds number equal to 43,000. The results showed a decrease in drag force coefficients with decreasing aspect ratio, as well as a decrease in Strouhal number with decreasing aspect ratio. The PIV showed the existence of an arch-type vortex originated in the cylinder free end.
New trends in earth sciences- Exploration of energy resourcesSwapnil Pal
A presentation on an article "strategies in geophysics: estimation of conventional and unconventional resources". Also a catchy analogy of a story "Nimboo pani" with role of a geologist in the current energy scenario.
Moisture content investigation in the soil samples using microwave dielectric...IJECEIAES
The microwaves of typical frequency ranges of 3 GHz to 30 GHz have been in use for remote sensing applications which are progressing rapidly. The microwaves can sense existing moisture in any material that absorbs moisture such as soil or vegetation. In case of soils which may be comprised of variable mix proportionate of solids, liquids or gases and distinct textures subjected to the associated size and the arrangements of soil particles. Hence, the moisture absorption by a specific type of soil used to be different. The inherent physical and electrical properties such as color, texture, grains, dielectric constant, conductivity or permeability, etc. differentiate various soils. In this work, authors present soil moisture measurement by simple estimation of emissivity i.e. the ratio of energy radiated by an object to absorbing the body of same physical temperature. A strategic method of measuring dielectric constant using a microwave signal is used in this research work. The measurement of the dielectric constant of the soils collected from the specific regions and analysis of results has been reported. The proposed method is less complex and can further be used for the identification of soil moisture and agricultural applications.
Pore scale dynamics and the interpretation of flow processes - Martin Blunt, Imperial College London, at UKCCSRC specialist meeting Flow and Transport for CO2 Storage, 29-30 October 2015
Report Of Evaporation Measuring Device.
Pan Evaporation or Pan Evaporimeter.
It consist of the seminar report for measurement of evaporation with use of pan of standard size.
International Journal of Engineering Research and Applications (IJERA) is an open access online peer reviewed international journal that publishes research and review articles in the fields of Computer Science, Neural Networks, Electrical Engineering, Software Engineering, Information Technology, Mechanical Engineering, Chemical Engineering, Plastic Engineering, Food Technology, Textile Engineering, Nano Technology & science, Power Electronics, Electronics & Communication Engineering, Computational mathematics, Image processing, Civil Engineering, Structural Engineering, Environmental Engineering, VLSI Testing & Low Power VLSI Design etc.
design specification and problems of kuraz irrigation schemetamasgenqmokonnin
project work on design specification and design ,construction and management problems of omo kuraz-1 sugar development project irrigation system. omo kuraz irrigation project construction was started since 2004 E,c . its for education purpose only
If you're not measuring water potential, or not measuring it correctly, your data could be telling you the wrong thing. Water content measurements can only tell you so much, and inferring water potential from water content is inaccurate at best, and completely misleading in worst-case scenarios.
In this 30-minute webinar, METER research scientist Leo Rivera discusses the good, the bad, and the ugly sides of measuring soil water potential. He'll walk you through the considerations and choices you need to take into account to select the perfect water potential sensor for your needs. Discover the challenges, limitations, and advantages of new sensor tech, and learn how to collect the most accurate measurements for your particular application.
Learn about:
- The large variety of technology available on the market
- The most recent trends and technologies
- Installation considerations and the tools available to make install better
- The limitations of using water content to infer water potential
- Our most recent research projects and findings
Similar to Ragab R 1 - UEI Day 1 - Kochi Jan18 (20)
Remote sensing to estimate the mean discharge of rivers from the Himalayan Foreland.
Kumar Gaurav (Indian Institute of Science Education and Research Bhopal Madhya Pradesh)
Welcome to TechSoup New Member Orientation and Q&A (May 2024).pdfTechSoup
In this webinar you will learn how your organization can access TechSoup's wide variety of product discount and donation programs. From hardware to software, we'll give you a tour of the tools available to help your nonprofit with productivity, collaboration, financial management, donor tracking, security, and more.
Instructions for Submissions thorugh G- Classroom.pptxJheel Barad
This presentation provides a briefing on how to upload submissions and documents in Google Classroom. It was prepared as part of an orientation for new Sainik School in-service teacher trainees. As a training officer, my goal is to ensure that you are comfortable and proficient with this essential tool for managing assignments and fostering student engagement.
How to Make a Field invisible in Odoo 17Celine George
It is possible to hide or invisible some fields in odoo. Commonly using “invisible” attribute in the field definition to invisible the fields. This slide will show how to make a field invisible in odoo 17.
Model Attribute Check Company Auto PropertyCeline George
In Odoo, the multi-company feature allows you to manage multiple companies within a single Odoo database instance. Each company can have its own configurations while still sharing common resources such as products, customers, and suppliers.
Palestine last event orientationfvgnh .pptxRaedMohamed3
An EFL lesson about the current events in Palestine. It is intended to be for intermediate students who wish to increase their listening skills through a short lesson in power point.
Acetabularia Information For Class 9 .docxvaibhavrinwa19
Acetabularia acetabulum is a single-celled green alga that in its vegetative state is morphologically differentiated into a basal rhizoid and an axially elongated stalk, which bears whorls of branching hairs. The single diploid nucleus resides in the rhizoid.
Read| The latest issue of The Challenger is here! We are thrilled to announce that our school paper has qualified for the NATIONAL SCHOOLS PRESS CONFERENCE (NSPC) 2024. Thank you for your unwavering support and trust. Dive into the stories that made us stand out!
2024.06.01 Introducing a competency framework for languag learning materials ...Sandy Millin
http://sandymillin.wordpress.com/iateflwebinar2024
Published classroom materials form the basis of syllabuses, drive teacher professional development, and have a potentially huge influence on learners, teachers and education systems. All teachers also create their own materials, whether a few sentences on a blackboard, a highly-structured fully-realised online course, or anything in between. Despite this, the knowledge and skills needed to create effective language learning materials are rarely part of teacher training, and are mostly learnt by trial and error.
Knowledge and skills frameworks, generally called competency frameworks, for ELT teachers, trainers and managers have existed for a few years now. However, until I created one for my MA dissertation, there wasn’t one drawing together what we need to know and do to be able to effectively produce language learning materials.
This webinar will introduce you to my framework, highlighting the key competencies I identified from my research. It will also show how anybody involved in language teaching (any language, not just English!), teacher training, managing schools or developing language learning materials can benefit from using the framework.
CLASS 11 CBSE B.St Project AIDS TO TRADE - INSURANCE
Ragab R 1 - UEI Day 1 - Kochi Jan18
1. IMPROVING IRRIGATION WATER
PRODUCTIVITY AND USE EFFICIENCY
USING NEW TECHNOLOGIES
RAGAB RAGAB1, RAG@CEH.AC.UK
CENTRE FOR ECOLOGY AND HYDROLOGY, CEH, UK
VICE PRESIDENT H., INTERNATIONAL COMMISSION ON IRRIGATION AND DRAINAGE, ICID
CONTRIBUTERS
EVANS1, J.G., BATTILANI2, A., AND SOLIMANDO2, D.
1. CENTRE FOR ECOLOGY AND HYDROLOGY, CEH, WALLINGFORD, OX10 8BB, UK
2. CONSORZIO DI BONIFICA DI SECONDO GRADO PER IL CANALE EMILIANO ROMAGNOLO – CER
2. “Integrating bio‐treated wastewater reuse and valorisation with
enhanced water use efficiency to support the Green Economy in
EU and India”.
Water4Crops
3. EU Consortium (21 Partners from 8 Countries):
5 Universities, 8 Research Institutes, 6 SMEs, 2 Consultant Comp.
TM SOLUTION LTD
4. W4Cs objectives
Valorizing agri-food-industry wastewater by recovering or producing
valuable chemicals
Increasing water availability by treating and reusing wastewater
Saving water in agriculture by enhancing water use efficiency through
• improved agronomics
• plant breeding
• innovative irrigation techniques
Enhancing stakeholders participation by co-creation process as well as through
Mirror Cases and INNOVA Platforms tools
5. Similar Structure
of EU and India W4Cs projects
WP5-I: Enabling green growth using water
treatment and reuse innovations (TERI)
WP6-I: Dissemination and
technology exchange (EIRC)
WP2-I: Municipal wastewater
biotreatment and reuse (NEERI)
13. Conclusion
When compared with RDI, the PRD irrigation
strategy in 2013, the potato used 15% less
irrigation, in the year 2014, maize received
17% less irrigation, in 2015, PRD received 28%
less water. The yield obtained under PRD was
equal or insignificantly less than RDI.
14. Towards accurate estimation of
crop water requirement without
the crop coefficient: new
approach using modern
technologies
19. What is scintillation?
Refractive index changes because of air
density differences – heat and moisture.
a typical scintillometer path
Transmitter
Receiver, measures
‘heat shimmer’
Atmospheric Turbulence Changes Air Density
infrared light and radio-waves
6 km Path length
Infra-red Light
Transmitter
20. 0.00
1.00
2.00
3.00
4.00
5.00
6.00
7.00
8.00
9.00
10.00
12/12/2013 22/03/2014 30/06/2014 08/10/2014 16/01/2015 26/04/2015 04/08/2015 12/11/2015
EVAPOTRANSPIRATION,MMDAY-1
Reference Evapotranspiration, ETo , Actual Evapotranspiration by Eddy Covariance, ETa
Eddy and by Scintillometer, ETa Scint
Eta Eddy ETa Scint ET0
Eta Eddy/Eto % Eta Scint/Eto %
44.46 34.38
Comparison between actual evapotranspiration measured by Eddy Covariance and by the Scintillometer versus the
reference evapotranspiration calculated by Penman-Monteith equation.
22. Actual evapotranspiration, ETa, measured by Eddy Covariance and the relative contribution of the crops within the
footprint to the total ETa for the 2014 season.
23. 0.00
2.00
4.00
6.00
8.00
10.00
12.00
12/12/2013 22/03/2014 30/06/2014 08/10/2014 16/01/2015 26/04/2015 04/08/2015 12/11/2015
EVAPOTRANSPIRATION,MMDAY-1
Reference Evapotranspiration, ETo, Crop Evapotranspiration, ETc , Actual
Evapotranspiration by Eddy Covariance, ETa Eddy and by Scintillometer, ETa Scint
Eta Eddy ETa Scint ET0 ETC
Eta Eddy/Eto % Eta Scint/Eto % Eta Eddy/Etc % Eta Scint/Etc %
44.46 34.38 45.14 34.91
Comparison between actual evapotranspiration measured by Eddy Covariance and Scintillometer, reference
evapotranspiration estimated from Penman-Monteith equation and crop evapotranspiration calculated from ETo and the
weighted mean of the crop coefficient Kc.
24. Conclusion
The ETc and ETo showed higher values than those of
ETa obtained by Eddy Covariance and Scintillometer.
On average the actual evapotranspiration of Eddy
Covariance and Scintillometers for the cropping
seasons 2014 and 2015 represented 45% and 35% of
the ETo and ETc, respectively. These are quite
significant differences.
25. • Calculating the reference evapotranspiration, ETo, or
the crop evapotranspiration, ETc, from meteorological
data, produces potential evapotranspiration that would
represent the atmospheric demand for water rather than
the crop demand for water.
• Accurate crop water requirement should be based on
crop and soil demand not on atmospheric demand for
water.
26. • Another benefit is, these modern technologies of
measuring the actual evapotranspiration do not need the
crop coefficient Kc, obtaining Kc is a major problem to
many irrigation practitioners.
• Other methods for measuring actual evaporation can
also be useful (e.g. weighing lysimeters, etc.).
• Short term monitoring of actual evaporation could be
used to derive a relationship with the commonly used
Eto or Etp that are easily obtainable from the standard
weather stations.
27. ESTIMATING CROP WATER REQUIREMENT
USING THE COSMIC-RAY SOIL MOISTURE
OBSERVATION SYSTEM (COSMOS)
http://cosmos.ceh.ac.uk/
29. College Field Top Transect
Sheepdrove Farm
21-04-2006
64 electrode ERT transect at
0.5m spacing crossing 3
distinct vegetation types –
winter cereal (foreground),
‘beetle-belt’ (centre), spring
cereal (distance)
30. College Top
21 April 2006
23 Aug 2006
Winter Barley Compacted Grass Beetle Belt Compacted Grass Spring Wheat
(Short) (Long)
0.2 0.25 0.3 0.35 0.4 0.45
10 (cm)
20 (cm)
30 (cm)
40 (cm)
50 (cm)
60 (cm)
80 (cm)
100 (cm)
120 (cm)
140 (cm)
160 (cm)
180 (cm)
200 (cm)
230 (cm)
NPDepth
Soil Moisture Fraction
Aug
April
31. COSMOS soil moisture sensors
• Large scale: 300-700 m radius of
sensitivity
• Non-invasive, completely passive
• Uses background fast neutrons
generated by Cosmic rays, which
are scattered (slowed) by H
atoms.
35. The volumetric soil moisture content, θ (m3 m-3) was calculated using
Desilets et al. (2010) analytically derived equation: The neutron counting
rate (counts hr-1), N, the corrected neutron counting rate over dry soil
under the same reference conditions, No, Three fitting parameter factors
that control the shape the soil moisture-neutron count rate relation, ao,
a1, and a2, being 0.0808, 0.372 and 0.115, respectively. No is determined
by field volumetric sampling and laboratory analysis within the Cosmos
footprint. 𝜽𝜽 𝑵𝑵 =
𝒂𝒂𝒂𝒂
𝑵𝑵
𝑵𝑵𝑵𝑵
−𝒂𝒂𝟏𝟏
− 𝒂𝒂𝒂𝒂
36. The effective depth of Cosmos measurement is defined as the thickness of
soil from which 86% of counted neutrons arise (Zreda et al., 2008).
The effective depth, z (cm), was calculated according to the hypothetical
equation of Franz et al. (2012) as:
𝒛𝒛 =
𝟓𝟓. 𝟖𝟖
𝝆𝝆 𝝉𝝉 + 𝜽𝜽 + 𝟎𝟎. 𝟎𝟎𝟎𝟎𝟎𝟎𝟎𝟎
37. The recorded data was transmitted in real time to the USA Cosmos web site:
http://Cosmos.hwr.arizona.edu/Probes/StationDat/098/index.php
38. Cosmos soil water content, effective depth and SMD for 2014-15 seasons. Cosmos water content was not adjusted for
biomass water content at this stage.
39. Cosmic ray probe calibration: Profile Probe access tubes distribution over the Cosmos probe dominated area in 2015.
http://www.water4crops.org/
40.
41. Cosmos soil water content after correction for biomass water content
42. Cosmos soil water content compared with cores soil moisture (0-50cm average) under all crops sprinkler and drip
irrigated in 2014-2015.
43. Cosmos soil water content compared with Profile probe soil moisture for plot 12 (100 m from Cosmos probe) at
different depths up to 100 cm.
44. Cosmos soil water content compared with Profile probe soil moisture averaged for all plots for 0-40 cm and 0-60cm
depths.
45. Cosmos soil water content compared with soil moisture sensors averaged for all plots and for 0-60 cm depth. 2014 cropping
season.
46. Cosmos soil water content compared with averaged soil moisture sensors, averaged soil cores and SALTMED
simulated soil moisture for maize, 2014 averaged for 0 -60 cm depth.
47. Method description Measurement details RMSE
Method
Measureme
nt
Year
Selected
plots
Number
of values
Depth, cm
No of
depths
averaged
Profile
probe
In situ-
2015
1 to 9 324 0-40 4 0.0426
Non-
continuous
1 to 9 405 0-60 5 0.0452
10, 11, 12 108 0-40 4 0.0363
10, 11, 12 135 0-60 5 0.0369
10 36 0-40 4 0.0384
10 45 0-60 5 0.0394
11 36 0-40 4 0.0356
11 45 0-60 5 0.0370
12 36 0-40 4 0.0374
12 45 0-60 5 0.0376
1 to 12 432 0-40 4 0.0330
1 to 12 540 0-60 5 0.0339
Sensors
In situ- 2014 4 plots 388 0-50 2 0.0423
continuous 2014-15 8 plots 792 0-50 2 0.0667
Soil cores Laboratory
2014-15 45 spots 930 0-50 5 0.0393
2015 40 spots 800 0-50 5 0.0290
Overall average 0.0394
48. Water content adjusted for biomass for 60 cm effective depth as verified and tested by field measurements.
49. Conclusion
• The Cosmos technology is one step in the right direction as it provides continuous,
integrated, area based values and solves the problem of spatial variability often found in
point measurements in relation to the soil spatial heterogeneity.
• This method could also be used to determine the soil moisture deficit, hence determine when
and how much to irrigate.
• The results showed that Cosmos soil moisture falls within the top 0-60 cm soil layer
verified by the soil moisture measured by sensors, soil cores and profile probes supported
by the SALTMED model. This indicates that there is a possibility that the Cosmos probe’s
effective depth could be within the top 0-60 cm of the irrigated lands.
50. • Knowing that almost 80% of the crop root system is accommodated within
the top 50-60 cm, the Cosmos measurement could be useful for
monitoring the soil water status and subsequently soil moisture deficit in
the root zone.
• The Cosmos technology could be made operational for irrigation managers
to determine when and how much to irrigate to avoid harmful water stress.
• In summary, these results support the use of Cosmos as an integrated area
based, non-destructive and hazard free method of measuring soil moisture
and for crop water requirement determination.