Difference between revisions of "Salinas Valley Seawater Intrusion"

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== Scientific Tools ==
 
== Scientific Tools ==
  
* The State of the Salinas River Groundwater Basin Report <ref name=SRGBR/> and Groundwater Extraction Summary Report <ref name=MCWRAGE>[http://www.co.monterey.ca.us/home/showdocument?id=24160 Monterey County Water Resource Association Groundwater Extraction April 2017 Summary Report]</ref>. developed by the MCWRA are useful tools for understanding how groundwater is utilized in the [[Salinas Valley]].
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* The State of the Salinas River Groundwater Basin Report <ref name=SRGBR/> and Groundwater Extraction Summary Report <ref name=MCWRAGE>[http://www.co.monterey.ca.us/home/showdocument?id=24160 Monterey County Water Resource Association Groundwater Extraction April 2017 Summary Report]</ref>, developed by the MCWRA, are useful tools for understanding how groundwater is utilized in the [[Salinas Valley]].
  
 
* Monitoring wells at selected sites within the Salinas Valley are tested to assess early indicators of seawater intrusion. Elevated sodium-to-chloride (Na/Cl) ratios indicate that numerous wells on the landward side of the seawater intrusion front have likely been affected, even though the chloride concentration has not increased to the 500 mg/L level used by MCWRA to delineate seawater intrusion.<ref name=SRGBR/>
 
* Monitoring wells at selected sites within the Salinas Valley are tested to assess early indicators of seawater intrusion. Elevated sodium-to-chloride (Na/Cl) ratios indicate that numerous wells on the landward side of the seawater intrusion front have likely been affected, even though the chloride concentration has not increased to the 500 mg/L level used by MCWRA to delineate seawater intrusion.<ref name=SRGBR/>

Revision as of 11:38, 28 March 2019

A watershed-related issue examined by the ENVS 560/L Watershed Systems class at CSUMB.

Seawater intrusion into groundwater aquifers from 1944 through 2015. The 180-Foot aquifer is one of two main water supply aquifers within the Salinas River Groundwater Basin. Images from Monterey County Water Resources Agency, made in 2017 [1]
Seawater intrusion into groundwater aquifers from 1944 through 2015. The 400-Foot aquifer is one of two main water supply aquifers within the Salinas River Groundwater Basin. Images from Monterey County Water Resources Agency, made in 2017 [2]

Summary

Seawater intrusion into the Salinas Valley groundwater aquifers has advanced since it was first measured in 1944.[3] In 2014 elevated salinity levels were recorded less than 1/2 mile from the city of Salinas at the 180-Foot aquifer[4], and seawater at that time was beginning to encroach beyond the limits of Castroville, CA at the 400-Foot aquifer. New maps indicate that these elevated salinity levels may have increased. The extent of seawater intrusion has moved farther inland due to continuing overdraft conditions for municipal and agricultural uses.

Location

The Salinas Valley basin is a groundwater basin beneath the Salinas Valley in California's Central Coast Region and is managed by the Salinas Valley Basin Groundwater Sustainability Agency. Groundwater is extracted from four major aquifers: Upper Valley, Forebay, East Side, and Pressure[5]. These aquifers create an interconnected groundwater system that supplies the bulk of the irrigation and municipal water usage in the Salinas Valley.

Hydrology

Along the coast of Monterey County, fresh groundwater flows from inland aquifers to meet with seawater from the ocean. The fresh groundwater flows from the Salinas Valley towards the coast where elevation and groundwater levels are lower. Due to the higher salinity of seawater, it is more dense than fresh groundwater and has a higher hydraulic head. When the fresh groundwater aquifers within the Salinas Valley have a lower hydraulic head, seawater moves inland in a wedge shape under freshwater until head levels return to equilibrium. Seawater and fresh groundwater then mix along the transition zone through dispersion and diffusion, raising salinity levels for wells that tap into these areas.[6] Once seawater intrusion has taken place, the effect on drinking and irrigation water quality within the aquifer is long-lasting. Wells are typically abandoned when salinity exceeds appropriate water quality standards.[7]

Stakeholders

There are a number of key stakeholders invested in groundwater resources such as the agriculture industry, businesses, government agencies, non-profits, and more. The following includes a brief overview of these stakeholder interests:

  • The agricultural industry is one key stakeholder within the Salinas Valley, as the estimated worth of the industry is $8.1 billion[8] and depends heavily on groundwater for almost all of its water needs[9]. Irrigation with high-salinity water damages crop yield, crop quality, and soil health for future use of the land for agriculture.[10]
  • Water providers in California's Central Coast Region have vested interests in the water management of areas such as Salinas, Castroville and Marina. The residents of these areas rely on the aquifers for urban use. When water salinity rises too high, it becomes unpalatable for drinking water and poses significant health threats.[11]

Laws, policies, & regulations

Seawater intrusion into groundwater aquifers from 1944 through 2013. The 180-Foot (left) and 400-Foot (right) aquifers are the two main water supply aquifers within the Salinas River Groundwater Basin. Images from State of the Salinas River Groundwater Basin Report (Jan. 2015) [12]

In 1961, Nacimiento Dam was completed to supply irrigation water to the Salinas Valley agricultural community and to recharge the aquifers. Attempts to change structural and operational practices at the dam have met severe local opposition resulting in several lawsuits[13]. A special act district, Monterey County Flood Control and Water Conservation District, was formed in 1947 for the Salinas Valley due to early concerns about seawater intrusion and flooding problems throughout the region. It later became the MCWRA in 1991, which monitors groundwater quality and levels[14] but has had little authority in regulating groundwater extraction. On September 16, 2014, Governor Jerry Brown signed into law a three-bill legislative package collectively known as the Sustainable Groundwater Management Act (SGMA). The SGMA mandates the formation of Groundwater Sustainability Agencies (GSA) and will significantly increase the role and responsibilities of local and state agencies to support sustainable groundwater management. As of March 2016, a draft plan has been developed for the GSA's key actions over the next several years that includes an outline for mitigating seawater intrusion.[15]

Water right laws are important in the management practices of this topic. A water right, as defined by the California Department of Fish and Wildlife is "legal permission to use a reasonable amount of water for a beneficial purpose such as swimming, fishing, farming or industry." [16] Water right laws are administered by the State Water Board's Division of Water Right. [17]

Mitigation Strategies

  • The Monterey County Water Recycling Projects were designed to retard seawater intrusion and protect drinking water supplies via wastewater recycling at a combined cost of $75 million. [18]
  • The Castroville Seawater Intrusion Project began construction in 1995 and started delivering recycled water to 12,000 acres of farmland near Castroville in 1998. By using recycled water pumped from the Monterey One Water plant, growers safely irrigate their crops and reduce pumping of seawater intruded groundwater.[19]
  • The Salinas Valley Reclamation Plant treats wastewater to advanced tertiary level. The resultant recycled water meets all California State Standards for recreational and irrigation uses. The facility can produce a maximum of 91 acre-feet per day. It is the largest sewage treatment installation in the world to recycle wastewater for freshly edible food crops.[19]
  • The Salinas Valley Water Project was a $33 million project designed to provide long-term management and protection of groundwater resources by stopping seawater intrusion and providing adequate water supplies and flexibility to meet needs in 2030.[20]
  • The Nacimiento Dam Spillway Modification Component enlarged the original spillway to increase the amount of flood flow that could be controlled by raising and strengthening chute walls and anchoring channel walls. Other modifications included the installation of an Obermeyer (rubber) Gate System and strengthening the bridge pier with steel reinforced concrete.[20]
  • The Salinas River Diversion Facility was constructed to provide treated (filtered and chlorinated) water from the Salinas River, significantly reducing the need to pump groundwater-except in periods of extremely high demand-through the use of a pneumatically controlled diversion dam.[20]
  • Phase II of the Salinas Valley Water Project has been proposed to construct two additional water capture and diversion facilities along the Salinas River. The two water diversion points will be located near Soledad and south of Salinas.[21] As of July 2014, MCWRA had requested resources to conduct an Environmental Impact Report and engaged in initial funding discussions[22].
  • Several other irrigation efficiency studies have been and are continuing to help reduce agricultural impact by reducing the quantity of water being applied to crops.[23][24]

Scientific Tools

  • The State of the Salinas River Groundwater Basin Report [12] and Groundwater Extraction Summary Report [5], developed by the MCWRA, are useful tools for understanding how groundwater is utilized in the Salinas Valley.
  • Monitoring wells at selected sites within the Salinas Valley are tested to assess early indicators of seawater intrusion. Elevated sodium-to-chloride (Na/Cl) ratios indicate that numerous wells on the landward side of the seawater intrusion front have likely been affected, even though the chloride concentration has not increased to the 500 mg/L level used by MCWRA to delineate seawater intrusion.[12]
  • Researchers at Stanford University use electrical resistivity tomography to noninvasive image depths of ~490 feet. Monitoring the electrical properties of water salinity along the the coast between Seaside and Marina provides a large area of coverage to map the location of seawater and fresh groundwater.[25]
  • The three-dimensional, finite-element-based Integrated Groundwater and Surface-Water Model (IGSM) was originally developed by Dr. Young S. Yoon in 1976 at the University of California, Los Angeles. Designed to simulate confined ground water flow, IGSM later underwent major revisions and modifications[26] including those made during application of IGSM to the Salinas Valley Integrated Groundwater and Surface-Water Model (SVIGSM)[27].
  • Modeling has been used to help understand Salinas Valley's groundwater hydrologic system. In her Senior Thesis at CSUMB, April McMillian used the SVIGSM to describe water table changes that have occurred due to water management policies[13].
  • RMC Water and Environment developed and calibrated an SVIGSM model and applied the criteria to the analysis of alternatives[28].

Ongoing Research

Compilation of paleo sea level data, tide gauge data, altimeter data, and estimates for likely projection range of global mean sea level rise scenarios, all relative to pre-industrial levels. Image sourced from IPCC Climate Change 2013[29]

Sea level rise must be included in future coastal aquifer studies due to probable impacts from global climate change. In 2013, the Intergovernmental Panel on Climate Change (IPCC) predicted about 1 meter of global mean sea level rise that will affect hydraulic head levels and seawater intrusion in Salinas Valley aquifers[29]:

  • Research conducted in the Department of Geography at UC Santa Barbara addressed the assessment of seawater intrusion potential from sea level rise in coastal aquifers of California. The Seaside Groundwater Basin, adjacent to the Salinas Valley aquifers, in Monterey County was simulated with sea-level rise of up to 0.9 meters using FEFLOW and ArcGIS as modeling and analytical tools.[30]

Managed aquifer recharge projects provide a method of increasing groundwater supply:

  • UC Santa Cruz researchers are involved in a series of studies on managed aquifer recharge using infiltration ponds in central coastal California. They aim to quantify variability in infiltration, recharge, groundwater movement, and water quality. Results suggest that managed recharge systems might be operated for simultaneous improvements to both water supply and quality.[31]

Irrigation management aims to reduce the amount of groundwater extracted for agricultural use and slow the rate of seawater intrusion:

  • The Terrestrial Observation and Prediction System (TOPS), a NASA modeling framework developed to monitor and forecast environmental conditions, is being developed to support the use of satellite data to provide rapid assessments of current crop conditions. The TOPS Satellite Irrigation Management Support web interface project will translate the satellite data into formats that are useful to agricultural producers in maximizing irrigation efficiency[32].
  • CropManage, a UC Cooperative Extension web application, starting in 2012, began development of evapotranspiration data from the California Irrigation Management and Information System to accurately estimate the appropriate applied irrigation to meet crop needs and minimize potential leaching losses of nitrates. The online interface is directed toward growers to track irrigation and nitrogen fertilizer schedules based on field trials of high-yield production crops.[33]

Groundwater level monitoring provides insight into the quantity of groundwater being extracted within the Salinas Valley:

  • MCWRA actively monitors key wells for monthly fluctuations, and annually measures an established network of wells to determine relative changes in groundwater storage. A survey is also conducted each August to monitor changes in coastal groundwater zones that will affect the inland movement of seawater. In addition to these three surveys, the MCWRA maintains a network of dedicated monitoring wells instrumented with electronic data loggers that record data at regular intervals.[34]

References

  1. Monterey County Water Resources Agency 2017
  2. Monterey County Water Resources Agency 2017
  3. Bulletin No. 52-B Salinas Basin Investigation Summary Report
  4. Historic Seawater Intrusion Map for Pressure 180-Foot Aquifer
  5. 5.0 5.1 MCWRA 2015 Summary Report
  6. USGS, 1964. Groundwater Resources Program: Saltwater Intrusion https://water.usgs.gov/ogw/gwrp/saltwater/salt.html
  7. USGS: Saltwater intrusion in coastal regions of North America
  8. MIIS: Agriculture Contributes $8.1 Billion to Local Economy
  9. Salinas Valley Water Project Description
  10. Pajaro Valley plan targets seawater intrusion
  11. NOAA: Can humans drink seawater?
  12. 12.0 12.1 12.2 State of the Salinas River Groundwater Basin Report (Jan. 2015)
  13. 13.0 13.1 Water Table Elevations in the Salinas Valley, California: Animated Visualization using GIS by April McMillian
  14. Monterey County Water Resources Agency Act
  15. California Department of Water Resources: Groundwater Sustainability Program Draft
  16. California Department of Fish and Wildlife on Water Rights
  17. California State Water Resources Control Board Division of Water Rights - Water Rights Programs Main Page
  18. Monterey One Water, 2017. Recycled Water. http://montereyonewater.org/facilities_tertiary_treatment.html
  19. 19.0 19.1 Marine Coast Water District: Recycled Water
  20. 20.0 20.1 20.2 MCWRA: Salinas Valley Water Project (SVWP) Overview
  21. MCWRA: Salinas Valley Water Project Phase II Overview
  22. MCWRA: Salinas Valley Water Project Phase II Project Status
  23. Sustainable Agriculture Research and Education: Building Tools and Technical Capacity to Improve Irrigation and Nutrient Management on California's Central Coast
  24. UC Cooperative Extension: Irrigation, Water Quality & Water Policy
  25. Stanford University: Imaging Saltwater Intrusion Along The Monterey Coast
  26. Review of the integrated groundwater and surface-water model (IGSM)
  27. MCWRA: Salinas Valley Integrated Ground Water and Surface Model Update
  28. Salinas Valley Integrated Regional Water Management Functionally Equivalent Plan Summary Document UPDATE
  29. 29.0 29.1 IPCC Climate Change 2013: The Physical Science Basis chapter 13
  30. Sea Water Intrusion by Sea-Level Rise: Scenarios for the 21st Century by Hugo A. Loaiciga, Thomas J. Pingel, and Elizabeth S. Garcia
  31. California Institute for Water Resources: Improving groundwater recharge
  32. TOPS Satellite Irrigation Management Support
  33. CropManage Overview: A web application for managing water and nitrogen fertilizer in lettuce
  34. MCWRA: Groundwater Level Monitoring Overview

Links

Disclaimer

This page may contain student work completed as part of assigned coursework. It may not be accurate. It does not necessary reflect the opinion or policy of CSUMB, its staff, or students.