Subsurface Drainage
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Groundwater Recharge from a Changing Landscape
ST. ANTHONY FALLS LABORATORY Engineering, Environmental and Geophysical Fluid Dynamics Project Report No. 490 Groundwater Recharge from a Changing Landscape by Timothy Erickson and Heinz G. Stefan Prepared for Minnesota Pollution Control Agency St. Paul, Minnesota May, 2007 Minneapolis, Minnesota The University of Minnesota is committed to the policy that all persons shall have equal access to its programs, facilities, and employment without regard to race, religion, color, sex, national origin, handicap, age or veteran status. 2 Abstract Urban development of rural and natural areas is an important issue and concern for many water resource management organizations and wildlife organizations. Change in groundwater recharge is one of the many effects of urbanization. Groundwater supplies to streams are necessary to sustain cold water organisms such as trout. An investigation of the changes of groundwater recharge associated with urbanization of rural and natural areas was conducted. The Vermillion River watershed, which is both a world class trout stream and on the fringes of the metro area of Minneapolis and St. Paul, Minnesota, was used for a case study. Substantial changes in groundwater recharge could destroy the cold water habitat of trout. In this report we give first an overview of different methods available to estimate recharge. We then present in some detail two models to quantify the changes in recharge that can be expected in a developing area. We finally apply these two models to a tributary watershed of the Vermillion River. In this report we discuss several techniques that can be used to estimate groundwater recharge: (1) the recession-curve-displacement method and (2) the base-flow-separation method that both use only streamflow records (Rutledge 1993, Lee and Chen 2003); (3) a recharge map developed by the USGS for the state of Minnesota (Lorenz and Delin 2007); (4) a minimal recharge map developed by the Minnesota Geological Survey using statistical methods (Ruhl et al. -
Land Use Change, Modelling of Soil Salinity And
KWAME NKRUMAH UNIVERSITY OF SCIENCE AND TECHNOLOGY, KUMASI, GHANA LAND USE CHANGE, MODELLING OF SOIL SALINITY AND HOUSEHOLDS’ DECISIONS UNDER CLIMATE CHANGE SCENARIOS IN THE COASTAL AGRICULTURAL AREA OF SENEGAL BY Sophie THIAM (BSc. Natural Sciences, MSc. Natural Resources Management and Sustainable Development) A Thesis submitted to the Department of Civil Engineering, College of Engineering in partial fulfilment of the requirements for the degree of DOCTOR OF PHILOSOPHY in Climate Change and Land Use June, 2019 DECLARATION I hereby declare that this submission is my own work towards the PhD in Climate Change and Land Use and that, to the best of my knowledge, it contains no material previously published by another person, nor material which has been accepted for the award of any other degree of the University, except where due acknowledgment has been made in the text. Sophie Thiam (PG7281816) Signature…………………Date………………... Certified by: Prof. Nicholas Kyei-Baffour Signature…………….…….Date……………… Department of Agricultural and Biosystems Engineering Kwame Nkrumah University of Science and Technology (Supervisor) Dr. François Matty Signature................................Date………… Institut des Sciences De l’Environnement University Cheikh Anta Diop of Dakar (Supervisor) Dr. Grace B.Villamor Signature………………….Date…………… Centre for Resilience Communities University of Idaho (Supervisor) Prof. Samuel Nii Odai Signature………………..Date………………. Head of Department of Civil Engineering i ABSTRACT Soil salinity remains one of the most severe environmental problems in the coastal agricultural areas in Senegal. It reduces crop yields thereby endangering smallholder farmers’ livelihood. To support effective land management, especially in coastal areas where impacts of climate change have induced soil salinity and food insecurity, this study investigated the patterns and impacts of soil salinity in a coastal agricultural landscape by developing an Agent-Based Model (ABM) for Djilor District, Fatick Region, Senegal. -
Miami-Dade County Drainage and Canals Flood Complaint Form
MIAMI-DADE COUNTY DRAINAGE AND CANALS FLOOD COMPLAINT FORM Service Request # _____________ Complaint Date Time AM PM Resident/Complainant Name Address Telephone Nearest Street Intersection of Flooding or Location of Flooding Is this the first time you report this? Yes No If No, date PLEASE SELECT ONLY ONE (1) COMPLAINT TYPE AND ANSWER RELATED QUESTIONS FOR BETTER SERVICE Type of Complaint 302 Clogged Storm Drain Is the water on top of drain now? Yes No How long does it take for the water to drain? What is the exact location of the drain? Is the area a new development? Yes No Was there a recent drainage project in the area? Yes No 303 Standing Water (No Drain) How deep is the water? How hard did it rain? Light Moderate Heavy Is your property flooded? Yes No Is your property in a new development? Yes No Where is the nearest drain? Flooding/Standing Water (Localized) Is the water flooding the inside of your residence? Yes No Is the water in your driveway / swale? Yes No Is the water across the roadway? Yes No Is it affecting traffic? Yes No How long does the water remain after rainfall? Page 1 of 2 MIAMI-DADE COUNTY DRAINAGE AND CANALS FLOOD COMPLAINT FORM Canal Complaints Solid waste (floating debris, bottles, cans, etc.) present Aquatic vegetation overgrown Needs mowing / treating vegetation on canal bank Bank instability due to Erosion / Collapses are present Culvert cleaning needed Damaged culvert / Headwall Encroachment of Easement / Right of Way Cutting / trimming of trees on a canal Right of Way needed Damaged Guardrails / Fence Canal Signs damaged / down Other Other Nature of Complaint For more information, call (305) 372-6688 Page 2 of 2 . -
Salinity Management and Soil Amendments for Southwestern Pecan Orchards J.L
ARIZONA COOPERATIVE E TENSION College of Agriculture and Life Sciences AZ1411 Revised 10/11 SALINITY MANAGEMENT AND SOIL AMENDMENTS FOR SOUTHWESTERN PECAN ORCHARDS J.L. Walworth Introduction Managing salts in Southwestern pecan orchards can be a major 1.0 challenge for growers, due to limited soil permeability and/or 1219721972 low-quality irrigation water. However, effective, long-term salt 1319631963 management is essential for maintaining productivity of pecan 0.8 1219721972 orchards. The challenge is to effectively manage soil salinity and sodium (Na) in a cost-effective manner, using appropriate combinations of irrigation management, soil management, and 0.6 soil amendments. Formation of Soil Salinity 0.4 Many arid region soils naturally contain high concentrations of soluble salts, because soil weathering processes dependent 0.2 upon precipitation have not been sufficiently intense to leach RTD = -0.095 x ECe –1.09 salts out of soils. Irrigation water and fertilizers contain salts R = -0.89** that may contribute further to the problem. Poor soil drainage due to the presence of compacted layers (hardpans, plowpans, 0.0 caliche, and clay lenses), heavy clay texture, or sodium problems 0022446688 may prevent downward movement of water and salts, making implementation of soil salinity control measures difficult. ECe (dS/m) Adequate soil drainage, needed to allow leaching of water and salts below the root zone of the trees, is absolutely essential for Figure 1. Reduction in pecan relative trunk diameter with increasing soil effective management of soil salinity. salt concentrations. After Miyamoto, et al., Irrig. Sci. (1986) 7:83-95. The risk of soil salinity formation is always greater in fine- textured (heavy) soils than in coarse-textured soils. -
Pages 406 To
397 SOIL SALINITY CONTROL UNDER BARLEY CULTIVATION USING A LABORATORY DRY DRAINAGE MODEL Shahab Ansari 1,*, Behrouz Mostafazadeh-Fard 2, Jahangir Abedi Koupai3 Abstract The drainage of agricultural fields is carried out in order to control soil salinity and the water table. Conventional drainage methods such as lateral drainage and interceptor drains have been used for many years. These methods increase agriculture production; but they are expensive and often cause environmental contaminations. One of the inexpensive and more environmental friendly methods that can be used in arid and semi-arid regions to remove excess salts from irrigated lands to non- irrigated or fallow lands is dry drainage. In the dry drainage method, natural soil system and the evaporation of fallow land is used to control soil salinity and the water table of irrigated land. There are few studies about dry drainage concepts. it is also important to study soil salt changes over time because of salt movements from irrigated areas to non-irrigated areas especially under plant cultivation. In this study a laboratory model which is able to simulate dry drainage was used to investigate soil salts transport under barley cultivation. The model was studied during the barley growing season and for a constant water table. During the growing season soil salinities of irrigated and non-irrigated areas were measured at different time. The Results showed that dry drainage can control the soil salinity of an irrigated area. The excess salts leached from an irrigated area and accumulated in the non-irrigated area and the leaching rate changed over time. -
Sediment Transport Model for a Surface Irrigation System
Hindawi Publishing Corporation Applied and Environmental Soil Science Volume 2013, Article ID 957956, 10 pages http://dx.doi.org/10.1155/2013/957956 Research Article Sediment Transport Model for a Surface Irrigation System Damodhara R. Mailapalli,1 Narendra S. Raghuwanshi,2 and Rajendra Singh2 1 BiologicalSystemsEngineering,UniversityofWisconsin,Madison,WI53706,USA 2 Agricultural and Food Engineering Department, Indian Institute of Technology, Kharagpur 721302, India Correspondence should be addressed to Damodhara R. Mailapalli; [email protected] Received 16 March 2013; Revised 25 June 2013; Accepted 11 July 2013 Academic Editor: Keith Smettem Copyright © 2013 Damodhara R. Mailapalli et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Controlling irrigation-induced soil erosion is one of the important issues of irrigation management and surface water impairment. Irrigation models are useful in managing the irrigation and the associated ill effects on agricultural environment. In this paper, a physically based surface irrigation model was developed to predict sediment transport in irrigated furrows by integrating an irrigation hydraulic model with a quasi-steady state sediment transport model to predict sediment load in furrow irrigation. The irrigation hydraulic model simulates flow in a furrow irrigation system using the analytically solved zero-inertial overland flow equations and 1D-Green-Ampt, 2D-Fok, and Kostiakov-Lewis infiltration equations. Performance of the sediment transport model wasevaluatedforbareandcroppedfurrowfields.Theresultsindicated that the sediment transport model can predict the initial sediment rate adequately, but the simulated sediment rate was less accurate for the later part of the irrigation event. -
Problems of Salination of Land in Coastal Areas of India and Suitable Protection Measures
Government of India Ministry of Water Resources, River Development & Ganga Rejuvenation A report on Problems of Salination of Land in Coastal Areas of India and Suitable Protection Measures Hydrological Studies Organization Central Water Commission New Delhi July, 2017 'qffif ~ "1~~ cg'il'( ~ \jf"(>f 3mft1T Narendra Kumar \jf"(>f -«mur~' ;:rcft fctq;m 3tR 1'j1n WefOT q?II cl<l 3re2iM q;a:m ~0 315 ('G),~ '1cA ~ ~ tf~q, 1{ffit tf'(Chl '( 3TR. cfi. ~. ~ ~-110066 Chairman Government of India Central Water Commission & Ex-Officio Secretary to the Govt. of India Ministry of Water Resources, River Development and Ganga Rejuvenation Room No. 315 (S), Sewa Bhawan R. K. Puram, New Delhi-110066 FOREWORD Salinity is a significant challenge and poses risks to sustainable development of Coastal regions of India. If left unmanaged, salinity has serious implications for water quality, biodiversity, agricultural productivity, supply of water for critical human needs and industry and the longevity of infrastructure. The Coastal Salinity has become a persistent problem due to ingress of the sea water inland. This is the most significant environmental and economical challenge and needs immediate attention. The coastal areas are more susceptible as these are pockets of development in the country. Most of the trade happens in the coastal areas which lead to extensive migration in the coastal areas. This led to the depletion of the coastal fresh water resources. Digging more and more deeper wells has led to the ingress of sea water into the fresh water aquifers turning them saline. The rainfall patterns, water resources, geology/hydro-geology vary from region to region along the coastal belt. -
Acid Sulfate Soil Materials
Site contamination —acid sulfate soil materials Issued November 2007 EPA 638/07: This guideline has been prepared to provide information to those involved in activities that may disturb acid sulfate soil materials (including soil, sediment and rock), the identification of these materials and measures for environmental management. What are acid sulfate soil materials? Acid sulfate soil materials is the term applied to soils, sediment or rock in the environment that contain elevated concentrations of metal sulfides (principally pyriteFeS2 or monosulfides in the form of iron sulfideFeS), which generate acidic conditions when exposed to oxygen. Identified impacts from this acidity cause minerals in soils to dissolve and liberate soluble and colloidal aluminium and iron, which may potentially impact on human health and the environment, and may also result in damage to infrastructure constructed on acid sulfate soil materials. Drainage of peaty acid sulfate soil material also results in the substantial production of the greenhouse gases carbon dioxide (CO2) and nitrous oxide (N2O). The oxidation of metal sulfides is a function of natural weathering processes. This process is slow however, and, generally, weathering alone does not pose an environmental concern. The rate of acid generation is increased greatly through human activities which expose large amounts of soil to air (eg via excavation processes). This is most commonly associated with (but not necessarily confined to) mining activities. Soil horizons that contain sulfides are called ‘sulfidic materials’ (Isbell 1996; Soil Survey Staff 2003) and can be environmentally damaging if exposed to air by disturbance. Exposure results in the oxidation of pyrite. This process transforms sulfidic material to sulfuric material when, on oxidation, the material develops a pH 4 or less (Isbell 1996; Soil Survey Staff 2003). -
Drainage Water Management R
doi:10.2489/jswc.67.6.167A RESEARCH INTRODUCTION Drainage water management R. Wayne Skaggs, Norman R. Fausey, and Robert O. Evans his article introduces a series of the most productive in the world. Drainage needed. Drainage water management, or papers that report results of field ditches or subsurface drains (tile or plastic controlled drainage, emerged as an effec- T studies to determine the effec- drain tubing) are used to remove excess tive practice for reducing losses of N in tiveness of drainage water management water and lower water tables, improve traf- drainage waters in the 1970s and 1980s. (DWM) on conserving drainage water ficability so that field operations can be The practice is inherently based on the and reducing losses of nitrogen (N) to sur- done in a timely manner, prevent water fact that the same drainage intensity is face waters. The series is focused on the logging, and increase yields. Drainage is not required all the time. It is possible to performance of the DWM (also called also needed to manage soil salinity in irri- dramatically reduce drainage rates during controlled drainage [CD]) practice in the gated arid and semiarid croplands. some parts of the year, such as the winter US Midwest, where N leached from mil- Drainage has been used to enhance crop months, without negatively affecting crop lions of acres of cropland contributes to production since the time of the Roman production. Drainage water management surface water quality problems on both Empire, and probably earlier (Luthin may also be used after the crop is planted local and national scales. -
Subsurface Drip Irrigation (Sdi) Systems
NETAFIM USA SUBSURFACE DRIP IRRIGATION (SDI) SYSTEMS ADVANCED DRIP/MICRO IRRIGATION TECHNOLOGIES SUBSURFACE DRIP IRRIGATION QUALITY AND DEPENDABILITY FROM THE LEADERS IN DRIP IRRIGATION For over 50 years, growers world-wide have counted on Netafim for the most reliable, cost-effective and efficient ways to deliver water, nutrients and chemicals to their crops. This tradition continues with subsurface drip irrigation (SDI), the most advanced method for irrigating agricultural crops. With proper management of water and nutrients, a subsurface drip irrigation system can deliver maximum yields and optimal water use efficiencies. Drip irrigation, whether surface or subsurface, often results in increased production and yields as well as increased quality and uniformity. It provides more efficient use of the applied water resulting in substantial water savings. The flexibility of drip irrigation increases a grower’s ability to farm marginal land. WHAT IS SUBSURFACE DRIP IRRIGATION (SDI)? Subsurface drip irrigation is a variation on traditional drip irrigation where the dripline (tubing and drippers) is buried beneath the soil surface, rather than laid on the ground, supplying water directly to the roots. The depth and distance the dripline is placed depends on the soil type and the plant’s root structure. SDI is more than an irrigation system, it is a root zone management tool. Fertilizer can be applied to the root zone in a quantity when it will be most beneficial - resulting in greater use efficiencies and better crop performance. SUBSURFACE DRIP IRRIGATION (SDI) ADVANTAGES The key benefit of a surface micro-irrigation system is to apply low volumes of water and nutrients uniformly to every plant across the entire field. -
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. -
4. Drainage of Irrigated Lands
ARBA MINCH UNIVERSITY Water Technology Institute Faculty of Meteorology and Hydrology Course Name:-Irrigated Lands Hydrology Course Code:- MHH1403 CHAPTER FOUR DRAINAGE OF IRRIGATED LANDS Prepared by: Tegegn T.(MSc.) Hydrology Objectives of the chapter • By the end of the session, the student will able to: – Understand what we mean by Agricultural drainage – Understand causes of excess water in agricultural lands – Know Problems and effects of poor drainage – Understand need of drainage – Know different types of drainage 4/21/2020 2 4.1 Definition of Drainage • Good water management of an irrigation scheme not only requires proper water application but also a proper drainage system. • Agricultural drainage can be defined as the removal of excess surface water and/or the lowering of the groundwater table below the root zone in order to improve plant growth. 4/21/2020 3 Cont… Class activity • Be in group and discuss on following topics – Causes of excess water or rise of water table – What are the effects of poor drainage – Why drainage is needed? 4/21/2020 4 Causes of excess water or rise of WT: • Natural Causes: – Poor natural drainage of the subsoil – Submergence under floods – Deep percolation from rainfall – Drainage water coming from adjacent areas. • Artificial Causes: – High intensity of irrigated agriculture irrespective of the soil or subsoil – Heavy seepage losses from unlined canals – Enclosing irrigated fields with embankments – Non-maintenance of natural drainages or blocking of natural drainages channels by roads. – the extra water applied for the flushing away of 4/21/2020 salts from the root zone. 5 4.2 Problems and effects of poor drainage • Drainage problem could be: – Surface drainage problem ---- when excess water builds up the water table and reaches to the ground level (i.e.