The document outlines the agenda for a two-day environmental technical training program. Day 1 covers an introduction to stormwater concepts like the hydrologic cycle, soils, and pre/post-construction conditions. It also covers terminology, rational method calculations, and a field visit. Day 2 covers best management practices, infiltration, and another field visit. Key concepts discussed in more depth include the hydrologic cycle, soils classification, rational method calculations, and how development impacts stormwater runoff rates and volumes.
Over the last decade, demand for spring management has increased as traditional spring sources have started drying up or becoming contaminated. In response, communities, NGOs and state agencies began dedicated spring protection programmes. In the Himalayas, the State of Sikkim and organizations such as Central Himalayan Action and Research Group (CHIRAG) and People Science Institute (PSI) started identifying and protecting spring recharge areas around 2007. The difference between these programmes and many other previous efforts is that they went beyond supply-side improvements to focus on the use of hydrogeology to map springsheds for targeted interventions.
The Advanced Centre for Water Resources Development and Management (ACWADAM), a research and capacity-building organization comprised of hydrogeologists and other experts began lending their expertise and building capacity of stakeholders. ACWADAM provides technical support, training and materials in hydrogeology to all network partners as well as others in India and the region. Similar programmes began independently in most of the mountain regions of India. Arghyam, a funding organization that was supporting many of these programmes, noticed that these disparate initiatives shared commonalities despite geographic diversity. They thus organized and funded a meeting of these various organizations in June 2014, and the Springs Initiative was born.
The springs initiative aims to tackle the current water crisis and to ensure safe and sustainable access to water for all, by promoting responsible and appropriate management of aquifers, springsheds, and watersheds and conserving ecosystems in partnership with communities, governments and other stakeholders.
This presentation has been developed as a part of the springs initiative to promote an understanding of springs and their role in mountainous areas.
Over the last decade, demand for spring management has increased as traditional spring sources have started drying up or becoming contaminated. In response, communities, NGOs and state agencies began dedicated spring protection programmes. In the Himalayas, the State of Sikkim and organizations such as Central Himalayan Action and Research Group (CHIRAG) and People Science Institute (PSI) started identifying and protecting spring recharge areas around 2007. The difference between these programmes and many other previous efforts is that they went beyond supply-side improvements to focus on the use of hydrogeology to map springsheds for targeted interventions.
The Advanced Centre for Water Resources Development and Management (ACWADAM), a research and capacity-building organization comprised of hydrogeologists and other experts began lending their expertise and building capacity of stakeholders. ACWADAM provides technical support, training and materials in hydrogeology to all network partners as well as others in India and the region. Similar programmes began independently in most of the mountain regions of India. Arghyam, a funding organization that was supporting many of these programmes, noticed that these disparate initiatives shared commonalities despite geographic diversity. They thus organized and funded a meeting of these various organizations in June 2014, and the Springs Initiative was born.
The springs initiative aims to tackle the current water crisis and to ensure safe and sustainable access to water for all, by promoting responsible and appropriate management of aquifers, springsheds, and watersheds and conserving ecosystems in partnership with communities, governments and other stakeholders.
This presentation has been developed as a part of the springs initiative to promote an understanding of springs and their role in mountainous areas.
Over the last decade, demand for spring management has increased as traditional spring sources have started drying up or becoming contaminated. In response, communities, NGOs and state agencies began dedicated spring protection programmes. In the Himalayas, the State of Sikkim and organizations such as Central Himalayan Action and Research Group (CHIRAG) and People Science Institute (PSI) started identifying and protecting spring recharge areas around 2007. The difference between these programmes and many other previous efforts is that they went beyond supply-side improvements to focus on the use of hydrogeology to map springsheds for targeted interventions.
The Advanced Centre for Water Resources Development and Management (ACWADAM), a research and capacity-building organization comprised of hydrogeologists and other experts began lending their expertise and building capacity of stakeholders. ACWADAM provides technical support, training and materials in hydrogeology to all network partners as well as others in India and the region. Similar programmes began independently in most of the mountain regions of India. Arghyam, a funding organization that was supporting many of these programmes, noticed that these disparate initiatives shared commonalities despite geographic diversity. They thus organized and funded a meeting of these various organizations in June 2014, and the Springs Initiative was born.
The springs initiative aims to tackle the current water crisis and to ensure safe and sustainable access to water for all, by promoting responsible and appropriate management of aquifers, springsheds, and watersheds and conserving ecosystems in partnership with communities, governments and other stakeholders.
This presentation has been developed as a part of the springs initiative to promote an understanding of springs and their role in mountainous areas.
Sedimentation in Sotorage Projects- Challenges and Mitigation MeasuresTEJASWI SHARMA
This slideshare is brief introduction about the sedimentation encountered in storage projects (reservoir) with the mitigation measures that could be applied.
Planning & design of water conservation (water harvesting) structures by nave...NAVEEN PATEKAR
The site which is suitable for construction of particular structure and which satisfied the design aspects and fulfil the requirement after construction
The suitable sites for water harvesting structures can be identify with the help of Remote sensing and GIS.
SOIL TYPE
SLOPE
INFILTRATION
RUNOFF POTENTIAL
LAND COVER LAND USE
STREAM ORDER
Hydrological Cycle give knowledge about how water evaporate transpiration and precipitate in atmosphere...It is also give ratios and percentage of water stored in different region how we can utilize it from this cycle, It is complete study of Water cycle travelling in earths surface and sub-surface.
Over the last decade, demand for spring management has increased as traditional spring sources have started drying up or becoming contaminated. In response, communities, NGOs and state agencies began dedicated spring protection programmes. In the Himalayas, the State of Sikkim and organizations such as Central Himalayan Action and Research Group (CHIRAG) and People Science Institute (PSI) started identifying and protecting spring recharge areas around 2007. The difference between these programmes and many other previous efforts is that they went beyond supply-side improvements to focus on the use of hydrogeology to map springsheds for targeted interventions.
The Advanced Centre for Water Resources Development and Management (ACWADAM), a research and capacity-building organization comprised of hydrogeologists and other experts began lending their expertise and building capacity of stakeholders. ACWADAM provides technical support, training and materials in hydrogeology to all network partners as well as others in India and the region. Similar programmes began independently in most of the mountain regions of India. Arghyam, a funding organization that was supporting many of these programmes, noticed that these disparate initiatives shared commonalities despite geographic diversity. They thus organized and funded a meeting of these various organizations in June 2014, and the Springs Initiative was born.
The springs initiative aims to tackle the current water crisis and to ensure safe and sustainable access to water for all, by promoting responsible and appropriate management of aquifers, springsheds, and watersheds and conserving ecosystems in partnership with communities, governments and other stakeholders.
This presentation has been developed as a part of the springs initiative to promote an understanding of springs and their role in mountainous areas.
Sedimentation in Sotorage Projects- Challenges and Mitigation MeasuresTEJASWI SHARMA
This slideshare is brief introduction about the sedimentation encountered in storage projects (reservoir) with the mitigation measures that could be applied.
Planning & design of water conservation (water harvesting) structures by nave...NAVEEN PATEKAR
The site which is suitable for construction of particular structure and which satisfied the design aspects and fulfil the requirement after construction
The suitable sites for water harvesting structures can be identify with the help of Remote sensing and GIS.
SOIL TYPE
SLOPE
INFILTRATION
RUNOFF POTENTIAL
LAND COVER LAND USE
STREAM ORDER
Hydrological Cycle give knowledge about how water evaporate transpiration and precipitate in atmosphere...It is also give ratios and percentage of water stored in different region how we can utilize it from this cycle, It is complete study of Water cycle travelling in earths surface and sub-surface.
SWaRMA_IRBM_Module6_#4, Sediment management including landslide and river ban...ICIMOD
This presentation is the part of 12-day (28 January–8 February 2019) training workshop on “Multi-scale Integrated River Basin Management (IRBM) from the Hindu Kush Himalayan Perspective” organized by the Strengthening Water Resources Management in Afghanistan (SWaRMA) Initiative of the International Centre for Integrated Mountain Development (ICIMOD), and targeted at participants from Afghanistan.
Revised Universal Soil Loss Equation 2 (RUSLE2) is a computer-based erosion prediction model used to estimate soil erosion rates caused by water on agricultural lands. It is an updated version of the original RUSLE (Revised Universal Soil Loss Equation) developed by the United States Department of Agriculture (USDA) in the 1960s. RUSLE2 was developed to incorporate advancements in technology, data availability, and erosion science, making it a more comprehensive and accurate tool for predicting soil erosion.
Artificial Reefs by Kuddle Life Foundation - May 2024punit537210
Situated in Pondicherry, India, Kuddle Life Foundation is a charitable, non-profit and non-governmental organization (NGO) dedicated to improving the living standards of coastal communities and simultaneously placing a strong emphasis on the protection of marine ecosystems.
One of the key areas we work in is Artificial Reefs. This presentation captures our journey so far and our learnings. We hope you get as excited about marine conservation and artificial reefs as we are.
Please visit our website: https://kuddlelife.org
Our Instagram channel:
@kuddlelifefoundation
Our Linkedin Page:
https://www.linkedin.com/company/kuddlelifefoundation/
and write to us if you have any questions:
info@kuddlelife.org
Natural farming @ Dr. Siddhartha S. Jena.pptxsidjena70
A brief about organic farming/ Natural farming/ Zero budget natural farming/ Subash Palekar Natural farming which keeps us and environment safe and healthy. Next gen Agricultural practices of chemical free farming.
"Understanding the Carbon Cycle: Processes, Human Impacts, and Strategies for...MMariSelvam4
The carbon cycle is a critical component of Earth's environmental system, governing the movement and transformation of carbon through various reservoirs, including the atmosphere, oceans, soil, and living organisms. This complex cycle involves several key processes such as photosynthesis, respiration, decomposition, and carbon sequestration, each contributing to the regulation of carbon levels on the planet.
Human activities, particularly fossil fuel combustion and deforestation, have significantly altered the natural carbon cycle, leading to increased atmospheric carbon dioxide concentrations and driving climate change. Understanding the intricacies of the carbon cycle is essential for assessing the impacts of these changes and developing effective mitigation strategies.
By studying the carbon cycle, scientists can identify carbon sources and sinks, measure carbon fluxes, and predict future trends. This knowledge is crucial for crafting policies aimed at reducing carbon emissions, enhancing carbon storage, and promoting sustainable practices. The carbon cycle's interplay with climate systems, ecosystems, and human activities underscores its importance in maintaining a stable and healthy planet.
In-depth exploration of the carbon cycle reveals the delicate balance required to sustain life and the urgent need to address anthropogenic influences. Through research, education, and policy, we can work towards restoring equilibrium in the carbon cycle and ensuring a sustainable future for generations to come.
UNDERSTANDING WHAT GREEN WASHING IS!.pdfJulietMogola
Many companies today use green washing to lure the public into thinking they are conserving the environment but in real sense they are doing more harm. There have been such several cases from very big companies here in Kenya and also globally. This ranges from various sectors from manufacturing and goes to consumer products. Educating people on greenwashing will enable people to make better choices based on their analysis and not on what they see on marketing sites.
Characterization and the Kinetics of drying at the drying oven and with micro...Open Access Research Paper
The objective of this work is to contribute to valorization de Nephelium lappaceum by the characterization of kinetics of drying of seeds of Nephelium lappaceum. The seeds were dehydrated until a constant mass respectively in a drying oven and a microwawe oven. The temperatures and the powers of drying are respectively: 50, 60 and 70°C and 140, 280 and 420 W. The results show that the curves of drying of seeds of Nephelium lappaceum do not present a phase of constant kinetics. The coefficients of diffusion vary between 2.09.10-8 to 2.98. 10-8m-2/s in the interval of 50°C at 70°C and between 4.83×10-07 at 9.04×10-07 m-8/s for the powers going of 140 W with 420 W the relation between Arrhenius and a value of energy of activation of 16.49 kJ. mol-1 expressed the effect of the temperature on effective diffusivity.
2. Course Overview – First Day
Introduction to Stormwater (90 min)
Hydrologic Cycle
Terminology
Soils
Pre and Post Construction
Rational Method
Group Problem (30 min)
Water Quality
Field Visit
3. Course Overview – Second Day
Best Management Practices(90 min)
Hyrdologic Cycle
Soils
Design Concepts
Pre vs. Post Conditions
Group Problem (30 min)
Best Management Practices (90 min)
Infiltration
Group Problem (30 min)
Field Visit
4.
5.
6. Hydrologic Cycle
The Hydrologic Cycle is the continuous process of water
moving within the earth’s atmosphere, on the earth’s
surface, and within the earth’s subsurface.
Atmosphere –Water Vapor.
Reaches earth’s surface thru precipitation (rain, snow,
hail, and fog).
Enters the earth’s subsurface thru infiltration.
7. Hydrologic Cycle
Ref: MA DEP Hydrologic Handbook for Conservation Commissioners, 2002
8. Stormwater and the
Hydrologic Cycle
Concerns
Surface Runoff –Water from precipitation that flows
over the ground surface.
Groundwater Recharge – The water that infiltrates into
the ground.
9. Stormwater and
the Hydrologic Cycle
Runoff
Increased volume changes wetland ecosystems.
Increase flooding.
Increased erosion.
Recharge
Decreased groundwater available for surface water.
Decreased water available for drinking water.
10. Terminology (The language of
stormwater)
Stormwater – Stormwater is the water that runs off surfaces
such as rooftops, paved streets, highways, and parking lots.
It can also come from hard grassy surfaces like lawns, play
fields, and from graveled roads and parking lots.
Non-Point Source Pollution: Pollutants from many diffuse
sources. Nonpoint-source pollution is caused by rainfall or
snowmelt moving over and through the ground. As the
runoff moves, it picks up and carries away natural and
human-made pollutants, finally depositing them into
lakes, rivers, wetlands, coastal waters, and even
underground sources of drinking water.
11. Terminology (The language of
stormwater)
Runoff -Water from precipitation that flows over the
ground surface.
Recharge -The water that infiltrates into the ground.
Stormwater –
Best Management Practices (BMPs) - Activities or
structural improvements that help reduce the quantity and
improve the quality of stormwater runoff.
Impervious Surface or Cover: The characteristic of a
material which prevents the infiltration of liquid through
it. This may apply to roads, streets, parking lots, rooftops
and sidewalks.
12. Terminology (The language of
stormwater)
Watershed: Geographical area that drains to a specified
point on a water course, usually a confluence of streams
or rivers, can also be known as drainage area,
catchments, or a river basin.
Detention - Release of surface and storm water runoff
from the site at a slower rate than it is collected by the
drainage facility system, the difference being held in
temporary storage.
Drainage - The collection, conveyance, containment,
and/or discharge of surface and storm water runoff.
15. SOILS
Four hydrologic groups are used. In the definitions to follow, the infiltration rate
is the rate at which water enters the soil at the surface and which is controlled by
surface conditions. The hydrologic soil groups, as defined by NRCS are:
A. (Low runoff potential) Soils having high infiltration rates even when
thoroughly wetted and consisting chiefly of deep, well to excessively drained
sands or gravels.
B. Soils having moderate infiltration rates when thoroughly wetted and
consisting chiefly of moderately deep to deep, moderately well-to-well drained
soils with moderately fine to moderately coarse textures.
C. Soils having slow infiltration rates when thoroughly wetted and consisting
chiefly of soils with a layer that impedes downward movement of water, or
soils with moderately fine to fine texture.
D. (High runoff potential) Soils having very slow infiltration rates when
thoroughly wetted and consisting chiefly of clay soils with a high swelling
potential, soils with a permanent high water table, soils with a clay pan or clay
layer at or near the surface, and shallow soils over nearly impervious material.
16. SOILS
Hydrologic Soil Group Infiltration (Inches/Hour)
A Exceeds 5.7
B 5.7 to 1.4
C 1.4 to 0.14
D Less than 0.14
17. Infiltration Rates – Rule of thumb
Class A Soils – 5 to 8 in/hour: Sand, Loamy Sand,
Sandy Loam (well to excessively drained)
Class B Soils – 1 to 2 in/hour: silt loam, loam
(moderately to well drained)
Class C Soils – 0.1 to 0.5 in/hour: Sandy clay loams
(slow infiltration)
Class D Soils – no infiltration.
18. SOILS
Ref: MA DEP Hydrologic Handbook for Conservation Commissioners, 2002
25. What is a 100-year storm?
A 100-year storm refers to rainfall totals that have a one
percent probability of occurring at that location in that year.
Encountering a "100-year storm" on one day does not
decrease the chance of a second 100-year storm occurring in
that same year or any year to follow. In other words, there is
a 1 in 100 or 1% chance that a storm will reach this intensity
in any given year. Likewise, a 50-year rainfall event has a 1 in
50 or 2% chance of occurring in a year. In addition, each
locality has its own criteria for how much rain must fall
within 24 hours to classify as a particular rain event. See
chart below for other rainfall events.
26. What is a 100-year storm?
Storm Intervals and Probabilities
Occurrence
Interval (years)
Probability in
Any Year
Percent Chance
in Any Year
100 1 in 100 1%
50 1 in 50 2%
25 1 in 25 4%
10 1 in 10 10%
5 1 in 5 20%
2 1 in 2 50%
28. ESTIMATING RUNOFF QUANTITIES
Volume
A parking lot has an area equal to a football field. It is 360 feet long by 160
Feet wide. An inch of rain falls on the parking lot of a course of an hour.
a.) What is the volume in cubic feet?
b.) What is the volume in acre-feet?
c.) What is the volume in gallons?
a.) Volume = (360-feet)(160-feet)(1-inch) (1-foot/12-inches)
Volume = 4,800 cubic feet = a cube with 17 foot sides
b.) Volume = (4,800 cubic feet)(1 acre/43,560 square feet) = 0.11 acre-feet
c.) Volume = (4,800 cubic feet)(7.48 gallons/cubic foot) = 36,000 gallons
Three to Four large tankers.
29. RUNOFF RATE
The runoff rate is the volume of runoff from a watershed
over a period if time. Usually measured as cubic feet per
second.
Depends on:
Ground surface roughness
Slope
Distance of travel
Higher rates increase flooding and erosion.
30. Finding Runoff Rates
One way is the Rational Method. Watersheds less than
20 acres. Used to size pipes. Other methods are
available.
We will review the Rational Method to for the purposes
of determining what information is important.
31. Rational Method
Rational formula is:
q = C ∙ i ∙ A
q = Peak rate of runoff – cubic feet per second
C = Runoff coefficient
i = Rainfall intensity
A = Watershed area in acres
32. Rational Method
Determine Runoff coefficient.
Parking Lot – Use asphalt
streets 0.7 to 0.95. Use 0.85.
Sandy soils - .05 to 0.10
Use 0.10.
33. Rational Method
Intensity – Duration – Frequency
Curve
Pick a duration, and a frequency,
then determine amount of rain in
that time period.
34. Rational Method
Intensity – Duration – Frequency
Curve
Pick a duration, and a frequency,
then determine amount of rain in
that time period.
Duration– 1 hour.
35. Rational Method
Intensity – Duration – Frequency
Curve
Pick a duration, and a frequency,
then determine amount of rain in
that time period.
Duration– 1 hour.
Frequency – 2 years
36. Rational Method
Intensity – Duration – Frequency
Curve
Pick a duration, and a frequency,
then determine amount of rain in
that time period.
Duration– 1 hour.
Frequency – 2 years
Intensity – 1.2 Inches per hour
i = 1.2 in/hr
39. Problem
Site is 2 acres. The difference in elevation across site is 5
feet. The length of the site is 400 feet. The soil is sand.
It is currently a grassed area. It will all be paved as a
parking lot.
Determine slope = difference in slope/length
40. Problem
Site is 2 acres. The difference in elevation across site is 5
feet. The length of the site is 400 feet. The soil is sand.
It is currently a grassed area. It will all be paved as a
parking lot.
Determine slope = difference in slope/length
= 5 feet/400 feet
41. Problem
Site is 2 acres. The difference in elevation across site is 5
feet. The length of the site is 400 feet. The soil is sand.
It is currently a grassed area. It will all be paved as a
parking lot.
Determine slope = difference in slope/length
= 5 feet/400 feet
= 0.012 feet/foot or 1.2 %
42. Problem
Site is 2 acres. The difference in elevation across site is 5
feet. The length of the site is 400 feet. The soil is sand.
It is currently a grassed area. It will all be paved as a
parking lot.
Slope = 1.2%
43. Rational Method
Determine Runoff coefficient.
Parking Lot – Use asphalt
streets 0.7 to 0.95. Use 0.85.
Sandy soils, flat - .05 to 0.10
Use 0.10.
44. Problem
Site is 2 acres. The difference in elevation across site is 5
feet. The length of the site is 400 feet. The soil is sand.
It is currently a grassed area. It will all be paved as a
parking lot.
Slope = 1.2%
CExisting = 0.1 CProposed = 0.85
Area = 2 acres
45. Problem
Using the rainfall intensity previously provided.
qgrass = C∙i∙A
46. Problem
Using the rainfall intensity previously provided.
qgrass = C∙i∙A = 0.10
47. Problem
Using the rainfall intensity previously provided. Two
year, one hour storm.
qgrass = C∙i∙A = 0.10 ∙ 1.2 in/hour ∙
48. Problem
Using the rainfall intensity previously provided. Two
year, one hour storm.
qgrass = C∙i∙A = 0.10 ∙ 1.2 in/hour ∙ 2 Acres
49. Problem
Using the rainfall intensity previously provided. Two
year, one hour storm.
qgrass = C∙i∙A = 0.10 ∙ 1.2 in/hour ∙ 2 Acres
= 0.24 cfs
50. Problem
Using the rainfall intensity previously provided. Two
year, one hour storm.
qgrass = C∙i∙A = 0.10 ∙ 1.2 in/hour ∙ 2 Acres
= 0.24 cfs
qparking lot = C∙i∙A = 0.85 ∙ 1.2 in/hour ∙ 2 Acres
= 2.04 cfs
8.5 times more runoff
51. WATER QUALITY
Water is essential to human life and to the health of the
environment. As a valuable natural resource, it
comprises marine, estuarine, freshwater (river and lakes)
and groundwater environments, across coastal and
inland areas. Water has two dimensions that are closely
linked - quantity and quality. Water quality is commonly
defined by its physical, chemical, biological and
aesthetic (appearance and smell) characteristics. A
healthy environment is one in which the water quality
supports a rich and varied community of organisms and
protects public health. Water quality in a body of water
influences the way in which communities use the water.
52. WATER QUALITY
More specifically, the water may be used by the community
for:
1. supplying drinking water
2. recreation (swimming, boating)
3. irrigating crops and watering stock
4. industrial processes
5. navigation and shipping
6. production of edible fish, shellfish and crustaceans
7. protection of aquatic ecosystems
8. wildlife habitats
9. scientific study and education
56. Oil and Grease
Oils and greases are a common component of stormwater runoff
pollutants, primarily because there are so many common sources:
streets and highways, parking lots, food waste storage areas, heavy
equipment and machinery storage areas, and areas where
pesticides have been applied. The familiar sight of a rainbow-colored
puddle or trickling stream in parking lots, driveways, and
street gutters is a reminder of the presence of oils and greases in
stormwater runoff. Oils and greases can be petroleum-based or
food-related (such as cooking oils). No type of oil or grease belongs
in surface water. Oil and grease are known to be toxic to aquatic
organisms at relatively low concentrations; they can coat fish gills,
prevent oxygen from entering the water, and clog drainage facilities
(leading to increased maintenance costs and potential flooding
problems)
58. Metals
Many heavy metals, including lead, copper, zinc and
cadmium, are commonly found in urban runoff. Metals
can contaminate surface and ground waters and
concentrate in bottom sediments, presenting health
problems for fish and animals that eat from the bottom.
Reproductive cycles of bottom-dwelling species can be
severely reduced, and fish inhabiting such metal-contaminated
locations often exhibit lesions and
tumors. Metals can also contaminate drinking water
supplies. Industrial areas, scrap yards, paints, pesticides,
and fallout from automobile emissions are typical
sources of heavy metals in runoff.
59. Metals
Copper and other common heavy metal
dust are produced during normal
automobile use. These fine particulates
settled onto paved surfaces and add to
the vehicular impact.
60. Sediments
Sediment - often originating as topsoil, sand, and clay - is the most common
pollutant in stormwater runoff by volume and weight. Sediments readily wash off
paved surfaces and exposed earth during storms. Sediment may seem harmless
enough, but it poses serious problems in the water. Excess sediment
concentrations turn stream and lake water cloudy, making it less suitable for
recreation, fish life, and plant growth. Sediment is of particular concern in fish
bearing streams where it can smother trout and salmon eggs, destroy habitat for
insects (a food source for fish), and cover prime spawning areas. Uncontrolled
sediment can also clog storm drains, leading to increased private and public
maintenance costs and flooding problems. Sediment is also of concern because
many other pollutants including oils, metals, bacteria, and nutrients tend to
attach to soil particles. Therefore when sediments enter water they usually carry
other pollutants with them. Cleared construction sites and exposed earth are
generally the greatest contributors of soil particles in surface waters. Other
sources include erosion from agricultural lands, application of sand and salts to
icy roads, fallout from pressure washing and sandblasting operations, dirt from
equipment and vehicles, and dirt and grit from parking lots, driveways, and
sidewalks
62. Nutrients
Nutrients such as phosphorus and nitrogen are needed by plants to grow, but high levels can
be harmful to water quality. Excess nutrient levels can over-stimulate the growth of algae
and other aquatic plants, resulting in unpleasant odors, unsightly surface scums, and
lowered dissolved oxygen levels from plant decay. Nutrients are most likely to pose a
problem in slow moving water such as lakes or sluggish streams. Some forms of algae are
toxic to fish and other aquatic organisms and may even cause death in animals that drink
affected water. Algae can also cause taste and odors problems in drinking waters, foul-smelling
odor in ponds and lakes, and problems with clogged water intakes, drains, and
pipes. Heavy loading of nutrients into slow-moving waters can adversely affect many
beneficial uses of the water. Forms of nitrogen (ammonium), in combination with pH and
temperature variations, can cause water quality problems and be toxic to fish. This process
consumes large amounts of oxygen in the water and subsequently stresses or kills fish and
other aquatic organisms when oxygen levels are reduced. Ammonia toxicity, due to nitrogen
in its ammonium form, can harm fish and other aquatic organisms.
Fertilizers, animal wastes, failing septic systems, detergents, road deicing salts, automobile
emissions, and organic matter such as lawn clippings and leaves are all contributors to
excessive nutrient levels in urban and agricultural stormwater runoff.
64. Toxic Organic Compounds
Pesticides and PCBs are toxic organic compounds that are particularly dangerous
in the aquatic environment. Excessive application of insecticides, herbicides,
fungicides, and rodenticides, or application of any of these shortly before a storm,
can result in toxic pesticide chemicals being carried from agricultural lands,
construction sites, parks, golf courses, and residential lawns to receiving waters.
Many pesticide compounds are extremely toxic to aquatic organisms and can
cause fish kills. PCBs are a similar class of toxic organic compounds. They can
contaminate stormwater through leaking electrical transformers. PCBs can settle
in sediments of receiving waters and, like pesticide compounds, present a serious
toxic threat to aquatic organisms that come in contact with them. Many other
toxic organic compounds can also affect receiving waters. These toxic compounds
include phenols, glycol ethers, esters, nitrosamines, and other nitrogen
compounds. Common sources of these compounds include wood preservatives,
antifreeze, dry cleaning chemicals, cleansers, and a variety of other chemical
products. Like pesticides and PCBs these other toxic organic compounds can be
lethal to aquatic organisms.
66. Fecal Coliform Bacteria
Fecal coliform bacteria in water may indicate the
presence of pathogenic (disease-causing) bacteria and
viruses. Pet and other animal wastes, failing septic
systems, livestock waste in agricultural areas and on
hobby farms, and fertilizers can all contribute fecal
coliform bacteria. This can be a problem for treatment of
drinking water and can limit recreational use of a water
body. Bacterial contamination has led to closures of
numerous shellfish harvesting areas and public
swimming beaches in Puget Sound.
68. High Temperature
Rainfall falling on roofs and pavements
Which have been heated by the sun will
be heated by these surfaces. The high
temperatures of this runoff can be
lethal to fish and other creatures/.
69. The Problem
The
Solution
Conventional Development Smart Development
Reduce land clearing and grading costs
Reduced infrastructure costs
Protect regional water quality
Reduce stormwater runoff
Impacts on open space