Development of a Group Built Coupled Physical-Socio- Economic Modelling Framework for Soil Salinity Management in Agricultural Watersheds in Developing Countries
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Water Balances
On website waterlog.info Agricultural hydrology is the study of water balance components intervening in agricultural water management, especially in irrigation and drainage/ Illustration of some water balance components in the soil Contents • 1. Water balance components • 1.1 Surface water balance 1.2 Root zone water balance 1.3 Transition zone water balance 1.4 Aquifer water balance • 2. Speficic water balances 2.1 Combined balances 2.2 Water table outside transition zone 2.3 Reduced number of zones 2.4 Net and excess values 2.5 Salt Balances • 3. Irrigation and drainage requirements • 4. References • 5. Internet hyper links Water balance components The water balance components can be grouped into components corresponding to zones in a vertical cross-section in the soil forming reservoirs with inflow, outflow and storage of water: 1. the surface reservoir (S) 2. the root zone or unsaturated (vadose zone) (R) with mainly vertical flows 3. the aquifer (Q) with mainly horizontal flows 4. a transition zone (T) in which vertical and horizontal flows are converted The general water balance reads: • inflow = outflow + change of storage and it is applicable to each of the reservoirs or a combination thereof. In the following balances it is assumed that the water table is inside the transition zone. If not, adjustments must be made. Surface water balance The incoming water balance components into the surface reservoir (S) are: 1. Rai - Vertically incoming water to the surface e.g.: precipitation (including snow), rainfall, sprinkler irrigation 2. Isu - Horizontally incoming surface water. This can consist of natural inundation or surface irrigation The outgoing water balance components from the surface reservoir (S) are: 1. -
Basic Elements of Ground-Water Hydrology with Reference to Conditions in North Carolina by Ralph C Heath
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Basic Elements of Ground-Water Hydrology With Reference to Conditions in North Carolina By Ralph C Heath U.S. Geological Survey Water-Resources Investigations Open-File Report 80-44 Prepared in cooperation with the North Carolina Department of Natural^ Resources and Community Development Raleigh, North Carolina 1980 United States Department of the Interior CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. W. Menard, Director For Additional Information Write to: Copies of this report may be purchased from: GEOLOGICAL SURVEY U.S. GEOLOGICAL SURVEY Open-File Services Section Post Office Box 2857 Branch of Distribution Box 25425, Federal Center Raleigh, North Carolina 27602 Denver, Colorado 80225 Preface Ground water is one of North Carolina's This report was prepared as an aid to most valuable natural resources. It is the developing a better understanding of the primary source-of water supplies in rural areas ground-water resources of the State. It and is also widely used by industries and consists of 46 essays grouped into five parts. municipalities, especially in the Coastal Plain. The topics covered by these essays range from However, its use is not increasing in proportion the most basic aspects of ground-water to the growth of the State's population and hydrology to the identification and correction economy. Instead, the present emphasis in of problems that affect the operation of supply water-supply development is on large regional wells. The essays were designed both for self systems based on reservoirs on large streams. study and for use in workshops on ground- The value of ground water as a resource not water hydrology and on the development and only depends on its widespread occurrence operation of ground-water supplies. -
Development of Rainfall-Runoff Model Using Tank Model: Problems and Challenges in Province of Aceh, Indonesia
Aceh International Journal of Science and Technology, 2 (1): 26-36 April 2013 ISSN: 2088-9860 REVIEW Development of Rainfall-runoff Model Using Tank Model: Problems and Challenges in Province of Aceh, Indonesia Hairul Basri Faculty of Agriculture, Syiah Kuala University, Banda Aceh 23111, Indonesia Corresponding author: Email: [email protected] Abtstract - Rainfall-runoff model using tank model founded by Sugawara has been widely used in Asia. Many researchers use the tank model to predict water availability and flooding in a watershed. This paper describes the concept of rainfall-runoff model using tank model, discuss the problems and challenges in using of the model, especially in Province of Aceh, Indonesia and how to improve the outcome of simulation of tank model. Many factors affect the rainfall-runoff phenomena of a wide range of watershed include: soil types, land use types, rainfall, morphometry, geology and geomorphology, caused the tank model usefull only for concerning watershed. It is necessary to adjust some parameters of tank model for other watershed by recalibrating the parameters of the model. Rainfall runoff model using the tank model for a watershed scale is more reasonable focused on each sub-watershed by considering soil types, land use types and rainfall of the concerning watershed. Land use data can be enhanced by using landsat imagery or aerial photographs to support the validation the existing of land use type. Long term of observed discharges and rainfall data should be increased by set up the AWLR (Automatic Water Level Recorder) and rainfall stations for each of sub-watersheds. The reasonable tank model can be resulted not only by calibrating the parameters, but also by considering the observed and simulated infiltration for each soil and land use types of the concerning watershed. -
Hydrological Controls on Salinity Exposure and the Effects on Plants in Lowland Polders
Hydrological controls on salinity exposure and the effects on plants in lowland polders Sija F. Stofberg Thesis committee Promotors Prof. Dr S.E.A.T.M. van der Zee Personal chair Ecohydrology Wageningen University & Research Prof. Dr J.P.M. Witte Extraordinary Professor, Faculty of Earth and Life Sciences, Department of Ecological Science VU Amsterdam and Principal Scientist at KWR Nieuwegein Other members Prof. Dr A.H. Weerts, Wageningen University & Research Dr G. van Wirdum Dr K.T. Rebel, Utrecht University Dr R.P. Bartholomeus, KWR Water, Nieuwegein This research was conducted under the auspices of the Research School for Socio- Economic and Natural Sciences of the Environment (SENSE) Hydrological controls on salinity exposure and the effects on plants in lowland polders Sija F. Stofberg Thesis submitted in fulfilment of the requirements for the degree of doctor at Wageningen University by the authority of the Rector Magnificus Prof. Dr A.P.J. Mol in the presence of the Thesis Committee appointed by the Academic Board to be defended in public on Wednesday 07 June 2017 at 4 p.m. in the Aula. Sija F. Stofberg Hydrological controls on salinity exposure and the effects on plants in lowland polders, 172 pages. PhD thesis, Wageningen University, Wageningen, the Netherlands (2017) With references, with summary in English ISBN: 978-94-6343-187-3 DOI: 10.18174/413397 Table of contents Chapter 1 General introduction .......................................................................................... 7 Chapter 2 Fresh water lens persistence and root zone salinization hazard under temperate climate ............................................................................................ 17 Chapter 3 Effects of root mat buoyancy and heterogeneity on floating fen hydrology .. -
Dissertation Simulating the Fate And
DISSERTATION SIMULATING THE FATE AND TRANSPORT OF SALINITY SPECIES IN A SEMI- ARID AGRICULTURAL GROUNDWATER SYSTEM: MODEL DEVELOPMENT AND APPLICATION Submitted by Saman Tavakoli Kivi Department of Civil and Environmental Engineering In partial fulfillment of the requirements For the Degree of Doctor of Philosophy Colorado State University Fort Collins, Colorado Summer 2018 Doctoral Committee: Advisor: Ryan T. Bailey Co-Advisor: Timothy K. Gates Michael J. Ronayne Aditi Bhaskar Copyright by Saman Tavakoli Kivi 2018 All Rights Reserved ABSTRACT SIMULATING THE FATE AND TRANSPORT OF SALINITY SPECIES IN A SEMI- ARID AGRICULTURAL GROUNDWATER SYSTEM: MODEL DEVELOPMENT AND APPLICATION Many irrigated agricultural areas worldwide suffer from salinization of soil, groundwater, and nearby river systems. Increased salinity concentrations, which can lead to decreased crop yield, are due principally to the presence of salt minerals and high rates of evapotranspiration. High groundwater salt loading to nearby river systems also affects downstream areas when saline river water is diverted for additional uses. Irrigation-induced salinity is the principal water quality problem in the semi-arid region of the western United States due to the extensive background quantities of salt in rocks and soils. Due to the importance of the problem and the complex hydro-chemical processes involved in salinity fate and transport, a physically-based spatially-distributed numerical model is needed to assess soil and groundwater salinity at the regional scale. Although several salinity transport models have been developed in recent decades, these models focus on salt species at the small scale (i.e. soil profile or field), and no attempts thus far have been made at simulating the fate, storage, and transport of individual interacting salt ions at the regional scale within a river basin. -
Effects of Irrigation Performance on Water Balance: Krueng Baro Irri- Gation Scheme (Aceh-Indonesia) As a Case Study
DOI: 10.2478/jwld-2019-0040 © Polish Academy of Sciences (PAN), Committee on Agronomic Sciences JOURNAL OF WATER AND LAND DEVELOPMENT Section of Land Reclamation and Environmental Engineering in Agriculture, 2019 2019, No. 42 (VII–IX): 12–20 © Institute of Technology and Life Sciences (ITP), 2019 PL ISSN 1429–7426, e-ISSN 2083-4535 Available (PDF): http://www.itp.edu.pl/wydawnictwo/journal; http://www.degruyter.com/view/j/jwld; http://journals.pan.pl/jwld Received 07.12.2018 Reviewed 05.03.2019 Accepted 07.03.2019 Effects of irrigation performance on water balance: A – study design B – data collection Krueng Baro Irrigation Scheme (Aceh-Indonesia) C – statistical analysis D – data interpretation E – manuscript preparation as a case study F – literature search Azmeri AZMERI1) ABCDEF , Alfiansyah YULIANUR2) AD, Uli ZAHRATI3) BC, Imam FAUDLI4) BC 1) orcid.org/0000-0002-3552-036X; Universitas Syiah Kuala, Faculty of Engineering, Civil Engineering Department Jl. Tgk. Syeh Abdul Rauf No. 7, Darussalam – Banda Aceh 23111, Indonesia; e-mail: [email protected] 2) orcid.org/0000-0002-8679-1792; Universitas Syiah Kuala, Faculty of Engineering, Civil Engineering Department, Banda Aceh, Indonesia; e-mail: [email protected] 3) orcid.org/0000-0001-8665-8193; Office of River Region of Sumatra-I, Lueng Bata, Banda Aceh, Indonesia; e-mail: [email protected] 4) orcid.org/0000-0002-4944-3449; Hydrology and hydraulics consultant; e-mail: [email protected] For citation: Azmeri A., Yulianur A., Zahrati U., Faudli I. 2019. Effects of irrigation performance on water balance: Krueng Baro Irri- gation Scheme (Aceh-Indonesia) as a case study. -
Saltmod Estimation of Root-Zone Salinity Varadarajan and Purandara
79 Original scientific paper Received: October 04, 2017 Accepted: December 14, 2017 DOI: 10.2478/rmzmag-2018-0008 SaltMod estimation of root-zone salinity Varadarajan and Purandara Application of SaltMod to estimate root-zone salinity in a command area Uporaba modela SaltMod za oceno slanosti koreninske cone na namakalnih površinah Varadarajan, N.*, Purandara, B.K. National Institute of Hydrology, Visvesvarayanagar, Belgaum 590019, Karnataka, India * [email protected] Abstract Povzetek Waterlogging and salinity are the common features - associated with many of the irrigation commands of - Poplavljanje in slanost tal sta običajna pojava v mno surface water projects. This study aims to estimate the vljanju slanosti v koreninski coni na levem in desnem gih namakalnih projektih. V študiji poročamo o ugota root zone salinity of the left and right bank canal com- mands of Ghataprabha irrigation command, Karnataka, - obrežju kanala namakalnega območja Ghataprabhaza India. The hydro-salinity model SaltMod was applied delom SaltMod so uporabili na izbranih kmetijskih v Karnataki, v Indiji. Postopek določanja slanosti z mo to selected agriculture plots at Gokak, Mudhol, Bili- parcelah v okrajih Gokak, Mudhol, Biligi in Bagalkot gi and Bagalkot taluks for the prediction of root-zone - salinity and leaching efficiency. The model simulated vodnjavanja tal. V raziskavi so modelirali slanost v tal- za oceno slanosti koreninske cone in učinkovitosti od the soil-profile salinity for 20 years with and without nem profilu v razdobju 20 let ob prisotnosti podpovr- subsurface drainage. The salinity level shows a decline šinskega odvodnjavanja in brez njega. Slanost upada with an increase of leaching efficiency. The leaching efficiency of 0.2 shows the best match with the actu- vzporedno z naraščanjem učinkovitosti odvodnjavanja. -
12(1)Download
Volume 12 No. 1 ISSN 0022–457X January-March 2013 Contents Land capability classification in relation to soil properties representing bio-sequences in foothills of North India 3 – V. K. Upadhayaya, R.D. Gupta and Sanjay Arora Innovative design and layout of Staggered Contour Trenches (SCTs) leads to higher survival of 10 plantation and reclamation of wastelands – R.R. Babu and Purnima Mishra Prioritization of sub-watersheds for erosion risk assessment - integrated approach of geomorphological 17 and rainfall erosivity indices – Rahul Kawle, S. Sudhishri and J. K. Singh Assessment of runoff potential in the National Capital Region of Delhi 23 – Manisha E Mane, S Chandra, B R Yadav, D K Singh, A Sarangi and R N Sahoo Soil information system for assessment and monitoring of crop insurance and economic compensation 31 to small and marginal farming communities – a conceptual framework – S.N. Das Rainfall trend analysis: A case study of Pune district in western Maharashtra region 35 – Jyoti P Patil, A. Sarangi, D. K. Singh, D. Chakraborty, M. S. Rao and S. Dahiya Assessment of underground water quality in Kathurah Block of Sonipat district in Haryana 44 – Pardeep, Ramesh Sharma, Sanjay Kumar, S.K. Sharma and B. Rath Levenberg - Marquardt algorithm based ANN approach to rainfall - runoff modelling 48 – Jitendra Sinha, R K Sahu, Avinash Agarwal, A. R. Senthil Kumar and B L Sinha Study of soil water dynamics under bioline and inline drip laterals using groundwater and wastewater 55 – Deepak Singh, Neelam Patel, T.B.S. Rajput, Lata and Cini Varghese Integrated use of organic manures and inorganic fertilizer on the productivity of wheat-soybean cropping 59 system in the vertisols of central India – U.K. -
Irrigation Influence on Catchment Hydrology Modelling with Advanced Hydroinformatic Tools
Research Journal of Agricultural Science, 48 (1), 2016 IRRIGATION INFLUENCE ON CATCHMENT HYDROLOGY MODELLING WITH ADVANCED HYDROINFORMATIC TOOLS Erika BEILICCI, R. BEILICCI Politechnica University Timisoara, Department of Hydrotechnical Engineering George Enescu str. 1/A, Timisoara, [email protected] Abstract: Agriculture is a significant user of water resources in Europe, accounting for around 30 per cent of total water use. Because water is essential to plant growth, irrigation is essentially to overcome deficiencies in rainfall for growing crops. Irrigation is a basic determinant of agriculture because its inadequacies are the most powerful constraints on the increase of agricultural production. Irrigation was recognized for its protective role of insurance against the vagaries of rainfall and drought. But the irrigation, besides the positive effects, has a significant environmental impact. The environmental impacts of irrigation are variable and not well-documented; some environmental impacts can be very severe. The main types of environmental impact arising from irrigation appear to be: water pollution from nutrients and pesticides; damage to habitats and aquifer exhaustion by abstraction of irrigation water; intensive forms of irrigated agriculture displacing formerly high value semi-natural ecosystems; gains to biodiversity and landscape from certain traditional or ‘leaky’ irrigation systems in some localized areas; increased erosion of cultivated soils on slopes; salinization, or contamination of water by minerals, of groundwater sources; both negative and positive effects of large scale water transfers, associated with irrigation projects. Minor irrigation schemes within a catchment will normally have negligible influence on the catchment hydrology, unless transfer of water over catchment boundaries is involved. Large irrigation schemes may significantly affect the runoff and the groundwater recharge through local increases in evapotranspiration and infiltration as well as through operational and field losses. -
(SHUD): Numerical Modeling of Watershed Hydrology with The
https://doi.org/10.5194/gmd-2019-354 Preprint. Discussion started: 14 January 2020 c Author(s) 2020. CC BY 4.0 License. Solver for Hydrologic Unstructured Domain (SHUD): Numerical modeling of watershed hydrology with the finite volume method Lele Shu1, Paul Ullrich1, and Christopher Duffy2 1Department of Land, Air, and Water Resources, University of California, Davis, Davis, California 95616, USA 2Department of Civil and Environmental Engineering, Pennsylvania State University, University Park, Pennsylvania 16802, USA Correspondence: Lele Shu ([email protected]) Abstract. Hydrological modeling is an essential strategy for understanding natural flows, particularly where observations are lacking in either space or time, or where topographic roughness leads to a disconnect in the characteristic timescales of overland and groundwater flow. Consequently, significant opportunities remain for the development of extensible modeling systems that operate robustly across regions. Towards the development of such a robust hydrological modeling system, this 5 paper introduces the Solver for Hydrological Unstructured Domain (SHUD), an integrated multi-process, multi-scale, multi- timestep hydrological model, in which hydrological processes are fully coupled using the Finite Volume Method. The SHUD integrates overland flow, snow accumulation/melting, evapotranspiration, subsurface and groundwater flow, and river routing, while realistically capturing the physical processes in a watershed. The SHUD incorporates one-dimension unsaturated flow, two-dimension groundwater flow, and river channels connected with hillslopes via overland flow and baseflow. 10 This paper introduces the design of SHUD, from the conceptual and mathematical description of hydrological processes in a watershed to computational structures. To demonstrate and validate the model performance, we employ three hydrolog- ical experiments: the V-Catchment experiment, Vauclin’s experiment, and a study of the Cache Creek Watershed in northern California, USA. -
Thesis Modeling the Distribution Of
THESIS MODELING THE DISTRIBUTION OF MAJOR SALT IONS IN REGIONAL AGRICULTURAL GROUNDWATER AND SURFACE WATER SYSTEMS: MODEL CALIBRATION AND APPLICATION Submitted by Abdullah B. Javed Department of Civil and Environmental Engineering In partial fulfillment of the requirements For the Degree of Master of Science Colorado State University Fort Collins, Colorado Spring 2020 Master’s Committee: Advisor: Timothy K. Gates Co Advisor: Ryan T. Bailey Michael J. Ronayn Copyright by Abdullah B. Javed 2020 All Rights Reserved 2 ABSTRACT MODELING THE DISTRIBUTION OF MAJOR SALT IONS IN AGRICULTURAL GROUNDWATER AND SURFACE WATER SYSTEMS: MODEL DEVELOPMENT AND APPLICATION Irrigated lands in Colorado’s Lower Arkansas River Valley (LARV), like many irrigated agricultural areas worldwide, suffer from salinization of soil, groundwater, and adjacent river systems. Waterlogging and salinization are prevalent throughout the LARV, which have diminished the crop yields and threatened the long-term sustainability of irrigated agriculture. Increased salinity concentrations are primarily due to the presence of salt minerals and high rates of evapotranspiration in the LARV, coupled with inefficient irrigation practices. Shallow groundwater in the LARV drives saline groundwater back to the stream network, thereby degrading the surface water quality, which affects the downstream areas where it evapo- concentrates when saline water is diverted for additional use. The goal of the current study is to develop, calibrate and test a physically-based, spatially distributed numerical model to assess soil, groundwater and surface water salinity at a regional scale to better understand the baseline nature of the problem. Several salinity models have been developed in recent decades; however, no attempts thus far have been made at simulating the fate, storage, and transport of salt ions at a regional scale in both groundwater and streams within an irrigated stream-aquifer system. -
Appendix 3. the P-GBSD Model the Present Study
Appendix 3. The P-GBSD model The present study demonstrates the use of a coupled Physical-Group-Built System Dynamics Model (P-GBSDM) for shock scenario simulation and data extraction. This model was selected for the present study due to 1) its capacity to accurately represent complex socio-environmental systems as a result of its dynamically coupled structure and built-in feedback networks and 2) the participatory nature of model development, including variables and system level flow networks defined by local stakeholders. The P-GBSDM, built by Inam, Adamowski, and Malard of the present paper, was created by integrating the physical Spatial Agro Hydro Salinity Model (SAHYSMOD) with a participatory, group-built system dynamics model (GBSDM) consisting of social, environmental, and economic variables. The GBSDM is a participatory model and all of its assumptions (e.g. farmer perceptions, government loan pay-back ratio, sedimentation rate, farm water storage potential, surface water /groundwater use ratio, crop rotation etc.) were refined through interviews with local stakeholders. Moreover, constants/parameters were defined through discussions with scientists with the necessary and relevant expertise (e.g., irrigation engineers, land reclamation experts, research officers, modelers etc.).The overall participatory (GBSD) model and its structure, equations, development methodology, and component details are presented in Inam et al. (2017). Socioeconomic interdependencies and feedbacks were determined through the participatory model-building process (conducted by Inam, Adamowski and Malard of the present paper) with local stakeholders in the Rechna Doab basin of northeastern Pakistan (Inam et al., 2015). The participatory model-building approach used in the initial stages of P-GBSDM development involved the application of stakeholder-built causal loop diagrams (CLD).