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dc.contributor.author
Jackson, Robert B.  
dc.contributor.author
Jobbagy Gampel, Esteban Gabriel  
dc.date.available
2024-07-08T12:49:33Z  
dc.date.issued
2005-10  
dc.identifier.citation
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  
dc.identifier.issn
0027-8424  
dc.identifier.uri
http://hdl.handle.net/11336/239322  
dc.description.abstract
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.  
dc.format
application/pdf  
dc.language.iso
eng  
dc.publisher
National Academy of Sciences  
dc.rights
info:eu-repo/semantics/openAccess  
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/  
dc.subject
icy roads  
dc.subject
salty streams  
dc.subject.classification
Ciencias del Suelo  
dc.subject.classification
Agricultura, Silvicultura y Pesca  
dc.subject.classification
CIENCIAS AGRÍCOLAS  
dc.title
From icy roads to salty streams  
dc.type
info:eu-repo/semantics/article  
dc.type
info:ar-repo/semantics/artículo  
dc.type
info:eu-repo/semantics/publishedVersion  
dc.date.updated
2024-06-04T15:04:53Z  
dc.journal.volume
102  
dc.journal.number
41  
dc.journal.pagination
14487-14488  
dc.journal.pais
Estados Unidos  
dc.journal.ciudad
Washington DC  
dc.description.fil
Fil: Jackson, Robert B.. School Of Law ; Duke University;  
dc.description.fil
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  
dc.journal.title
Proceedings of the National Academy of Sciences of The United States of America  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/https://doi.org/10.1073/pnas.0507389102  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://www.pnas.org/doi/full/10.1073/pnas.0507389102