From icy roads to salty streams

Autores
Jackson, Robert B.; Jobbagy Gampel, Esteban Gabriel
Año de publicación
2005
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
For most of human history, saltwas a precious commodity. People prized it for flavoring and preserving food and for use in religious ceremonies and burials. The Roman occupation of Britain peppered the English language with a legacy of salt. We retain those Latin links in words such as ‘‘salary’’ and ‘‘salami’’ and in place names like Greenwich and Sandwich, their suffix denoting a saltworks. Today salt is no longer precious. The U.S. mines _36 million metric tons [1 metric ton _ 1 megagram (Mg)] of rock salt a year (1). Eighteen million Mg is spread on paved surfaces for deicing, making winter roads safer for people and vehicles (2). However, once the salt dissolves, it washes into streams or soil and is forgotten. A new article by Kaushal et al. (3) in a recent issue of PNAS suggested that it should not be. The use of rock salt (NaCl) on U.S. roads has skyrocketed in the last 65 years (Fig. 1), and chloride (Cl) concentrations in waters of the northeast have risen as a consequence (4–6). The mobility of salt in water leads to its potential problems in the environment. These problems include toxicity to plants and fish, groundwater contamination, and human health interactions, particularly salt intake and hypertension (7–9). In consequence, researchers have been monitoring increased salt concentrations in streams and groundwater for decades (4–6, 10). A second aspect is their intensive focus on streams in the greater Baltimore area. In this rapidly urbanizing region, they found a logarithmic relationship between the proportion of pavement in a watershed and the mean annual Cl concentration in streams observed in the northeastern U.S. and Canada (11, 12). For  example, a survey of 23 springs in the greater Toronto area found Cl concentrations topping 1,200 mg_liter_1 arising from road salt use (11). This groundwater salinity is the primary concern for long-term potable water supply. Once groundwater becomes salty, it typically will take decades to centuries for the salts to disappear, even when road salt use ends.
Fil: Jackson, Robert B.. School Of Law ; Duke University;
Fil: Jobbagy Gampel, Esteban Gabriel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - San Luis. Instituto de Matemática Aplicada de San Luis "Prof. Ezio Marchi". Universidad Nacional de San Luis. Facultad de Ciencias Físico, Matemáticas y Naturales. Instituto de Matemática Aplicada de San Luis "Prof. Ezio Marchi"; Argentina
Materia
icy roads
salty streams
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/239322

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spelling From icy roads to salty streamsJackson, Robert B.Jobbagy Gampel, Esteban Gabrielicy roadssalty streamshttps://purl.org/becyt/ford/4.1https://purl.org/becyt/ford/4For most of human history, saltwas a precious commodity. People prized it for flavoring and preserving food and for use in religious ceremonies and burials. The Roman occupation of Britain peppered the English language with a legacy of salt. We retain those Latin links in words such as ‘‘salary’’ and ‘‘salami’’ and in place names like Greenwich and Sandwich, their suffix denoting a saltworks. Today salt is no longer precious. The U.S. mines _36 million metric tons [1 metric ton _ 1 megagram (Mg)] of rock salt a year (1). Eighteen million Mg is spread on paved surfaces for deicing, making winter roads safer for people and vehicles (2). However, once the salt dissolves, it washes into streams or soil and is forgotten. A new article by Kaushal et al. (3) in a recent issue of PNAS suggested that it should not be. The use of rock salt (NaCl) on U.S. roads has skyrocketed in the last 65 years (Fig. 1), and chloride (Cl) concentrations in waters of the northeast have risen as a consequence (4–6). The mobility of salt in water leads to its potential problems in the environment. These problems include toxicity to plants and fish, groundwater contamination, and human health interactions, particularly salt intake and hypertension (7–9). In consequence, researchers have been monitoring increased salt concentrations in streams and groundwater for decades (4–6, 10). A second aspect is their intensive focus on streams in the greater Baltimore area. In this rapidly urbanizing region, they found a logarithmic relationship between the proportion of pavement in a watershed and the mean annual Cl concentration in streams observed in the northeastern U.S. and Canada (11, 12). For  example, a survey of 23 springs in the greater Toronto area found Cl concentrations topping 1,200 mg_liter_1 arising from road salt use (11). This groundwater salinity is the primary concern for long-term potable water supply. Once groundwater becomes salty, it typically will take decades to centuries for the salts to disappear, even when road salt use ends.Fil: Jackson, Robert B.. School Of Law ; Duke University;Fil: Jobbagy Gampel, Esteban Gabriel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - San Luis. Instituto de Matemática Aplicada de San Luis "Prof. Ezio Marchi". Universidad Nacional de San Luis. Facultad de Ciencias Físico, Matemáticas y Naturales. Instituto de Matemática Aplicada de San Luis "Prof. Ezio Marchi"; ArgentinaNational Academy of Sciences2005-10info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/239322Jackson, Robert B.; Jobbagy Gampel, Esteban Gabriel; From icy roads to salty streams; National Academy of Sciences; Proceedings of the National Academy of Sciences of The United States of America; 102; 41; 10-2005; 14487-144880027-8424CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1073/pnas.0507389102info:eu-repo/semantics/altIdentifier/url/https://www.pnas.org/doi/full/10.1073/pnas.0507389102info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T09:45:49Zoai:ri.conicet.gov.ar:11336/239322instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-03 09:45:49.273CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv From icy roads to salty streams
title From icy roads to salty streams
spellingShingle From icy roads to salty streams
Jackson, Robert B.
icy roads
salty streams
title_short From icy roads to salty streams
title_full From icy roads to salty streams
title_fullStr From icy roads to salty streams
title_full_unstemmed From icy roads to salty streams
title_sort From icy roads to salty streams
dc.creator.none.fl_str_mv Jackson, Robert B.
Jobbagy Gampel, Esteban Gabriel
author Jackson, Robert B.
author_facet Jackson, Robert B.
Jobbagy Gampel, Esteban Gabriel
author_role author
author2 Jobbagy Gampel, Esteban Gabriel
author2_role author
dc.subject.none.fl_str_mv icy roads
salty streams
topic icy roads
salty streams
purl_subject.fl_str_mv https://purl.org/becyt/ford/4.1
https://purl.org/becyt/ford/4
dc.description.none.fl_txt_mv For most of human history, saltwas a precious commodity. People prized it for flavoring and preserving food and for use in religious ceremonies and burials. The Roman occupation of Britain peppered the English language with a legacy of salt. We retain those Latin links in words such as ‘‘salary’’ and ‘‘salami’’ and in place names like Greenwich and Sandwich, their suffix denoting a saltworks. Today salt is no longer precious. The U.S. mines _36 million metric tons [1 metric ton _ 1 megagram (Mg)] of rock salt a year (1). Eighteen million Mg is spread on paved surfaces for deicing, making winter roads safer for people and vehicles (2). However, once the salt dissolves, it washes into streams or soil and is forgotten. A new article by Kaushal et al. (3) in a recent issue of PNAS suggested that it should not be. The use of rock salt (NaCl) on U.S. roads has skyrocketed in the last 65 years (Fig. 1), and chloride (Cl) concentrations in waters of the northeast have risen as a consequence (4–6). The mobility of salt in water leads to its potential problems in the environment. These problems include toxicity to plants and fish, groundwater contamination, and human health interactions, particularly salt intake and hypertension (7–9). In consequence, researchers have been monitoring increased salt concentrations in streams and groundwater for decades (4–6, 10). A second aspect is their intensive focus on streams in the greater Baltimore area. In this rapidly urbanizing region, they found a logarithmic relationship between the proportion of pavement in a watershed and the mean annual Cl concentration in streams observed in the northeastern U.S. and Canada (11, 12). For  example, a survey of 23 springs in the greater Toronto area found Cl concentrations topping 1,200 mg_liter_1 arising from road salt use (11). This groundwater salinity is the primary concern for long-term potable water supply. Once groundwater becomes salty, it typically will take decades to centuries for the salts to disappear, even when road salt use ends.
Fil: Jackson, Robert B.. School Of Law ; Duke University;
Fil: Jobbagy Gampel, Esteban Gabriel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - San Luis. Instituto de Matemática Aplicada de San Luis "Prof. Ezio Marchi". Universidad Nacional de San Luis. Facultad de Ciencias Físico, Matemáticas y Naturales. Instituto de Matemática Aplicada de San Luis "Prof. Ezio Marchi"; Argentina
description For most of human history, saltwas a precious commodity. People prized it for flavoring and preserving food and for use in religious ceremonies and burials. The Roman occupation of Britain peppered the English language with a legacy of salt. We retain those Latin links in words such as ‘‘salary’’ and ‘‘salami’’ and in place names like Greenwich and Sandwich, their suffix denoting a saltworks. Today salt is no longer precious. The U.S. mines _36 million metric tons [1 metric ton _ 1 megagram (Mg)] of rock salt a year (1). Eighteen million Mg is spread on paved surfaces for deicing, making winter roads safer for people and vehicles (2). However, once the salt dissolves, it washes into streams or soil and is forgotten. A new article by Kaushal et al. (3) in a recent issue of PNAS suggested that it should not be. The use of rock salt (NaCl) on U.S. roads has skyrocketed in the last 65 years (Fig. 1), and chloride (Cl) concentrations in waters of the northeast have risen as a consequence (4–6). The mobility of salt in water leads to its potential problems in the environment. These problems include toxicity to plants and fish, groundwater contamination, and human health interactions, particularly salt intake and hypertension (7–9). In consequence, researchers have been monitoring increased salt concentrations in streams and groundwater for decades (4–6, 10). A second aspect is their intensive focus on streams in the greater Baltimore area. In this rapidly urbanizing region, they found a logarithmic relationship between the proportion of pavement in a watershed and the mean annual Cl concentration in streams observed in the northeastern U.S. and Canada (11, 12). For  example, a survey of 23 springs in the greater Toronto area found Cl concentrations topping 1,200 mg_liter_1 arising from road salt use (11). This groundwater salinity is the primary concern for long-term potable water supply. Once groundwater becomes salty, it typically will take decades to centuries for the salts to disappear, even when road salt use ends.
publishDate 2005
dc.date.none.fl_str_mv 2005-10
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/239322
Jackson, Robert B.; Jobbagy Gampel, Esteban Gabriel; From icy roads to salty streams; National Academy of Sciences; Proceedings of the National Academy of Sciences of The United States of America; 102; 41; 10-2005; 14487-14488
0027-8424
CONICET Digital
CONICET
url http://hdl.handle.net/11336/239322
identifier_str_mv Jackson, Robert B.; Jobbagy Gampel, Esteban Gabriel; From icy roads to salty streams; National Academy of Sciences; Proceedings of the National Academy of Sciences of The United States of America; 102; 41; 10-2005; 14487-14488
0027-8424
CONICET Digital
CONICET
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language eng
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dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
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