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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Arctic Ocean
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Norwegian Sea (1)
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Arctic region
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Greenland (1)
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Asia
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Indian Peninsula
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India
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Tamil Nadu India (1)
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Chalk Aquifer (1)
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Europe
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Sjaelland (1)
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elements, isotopes
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metals
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lead
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Pb-208/Pb-206 (1)
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mercury (1)
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geologic age
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Paleozoic
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vermiculite (1)
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mica group (1)
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rectorite (1)
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Primary terms
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Arctic Ocean
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Norwegian Sea (1)
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Arctic region
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Greenland (1)
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Asia
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Indian Peninsula
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India
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Tamil Nadu India (1)
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-
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Cenozoic
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Quaternary (1)
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Tertiary
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Paleogene
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Eocene
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upper Eocene (1)
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Oligocene
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lower Oligocene (1)
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clay mineralogy (4)
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Europe
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Germany (1)
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Rhine Valley (1)
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Scandinavia
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Denmark
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Sjaelland (1)
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England (1)
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geochemistry (9)
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ground water (12)
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isotopes
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stable isotopes
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Pb-208/Pb-206 (1)
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land use (1)
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metals
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lead
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mercury (1)
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Mexico
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Mexico state
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Federal District Mexico
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Mexico City Mexico (1)
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minerals (1)
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Ocean Drilling Program
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Leg 104
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ODP Site 643 (1)
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Leg 151
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ODP Site 913 (1)
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Leg 162
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ODP Site 985 (1)
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paleoclimatology (1)
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Paleozoic
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Carboniferous
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Pennsylvanian
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Middle Pennsylvanian (1)
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Devonian
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Upper Devonian
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Cleveland Member (1)
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Famennian (1)
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Ohio Shale (1)
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palynomorphs
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miospores
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pollen (1)
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pollution (13)
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sedimentary rocks
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carbonate rocks
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chalk (1)
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sediments
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clastic sediments
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loess (2)
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marine sediments (2)
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soils (7)
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United States
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California
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Los Angeles County California
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Los Angeles California (1)
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Ventura County California (2)
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Eastern U.S. (1)
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Illinois
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DeKalb County Illinois (2)
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Kentucky
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Eastern Kentucky coal field (1)
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Midwest (1)
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Western U.S. (1)
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Wyoming (1)
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-
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sedimentary rocks
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sedimentary rocks
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carbonate rocks
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chalk (1)
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-
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sediments
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sediments
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clastic sediments
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loess (2)
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marine sediments (2)
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-
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soils
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soils (7)
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ethers
The use of glycol ethers to help reduce amorphous organic matter (AOM) in palynological preparations
Gel polymer electrolyte based on poly(methyl methacrylate-maleic anhydride)-poly(ethylene glycol) monomethyl ether and organophilic rectorite clay
Chamosite, a naturally occurring clay as a versatile catalyst for various organic transformations
Assessment of the use of fluorescent tracers in a contaminated Chalk aquifer
Onset of long-term cooling of Greenland near the Eocene-Oligocene boundary as revealed by branched tetraether lipids
Influence of ethanol and methyl tert-butyl ether on the biodegradation and transport of benzene in loess
Sorption of methyl tert-butyl ether and benzene in fine-grained materials from northern Illinois and the Chalco Basin, Mexico
Simultaneous high throughput and quantitative analysis of MTBE and BTEX by P&T-GCMS using a Precept® autosampler
SORPTION OF A NONIONIC POLYOXYETHYLENE LAURYL ETHER SURFACTANT BY 2:1 LAYER SILICATES
Abstract Human activities impact an estimated 98% of rivers in the United States. This chapter summarizes impacts associated with pioneer societies, commercial activities, and public works. In pioneer societies, individuals or small groups undertake activities such as timber harvest, agriculture, or navigation improvements. Nineteenth-century placer mining of gold along rivers of California's Sierra Nevada is used as a case study. Commercial activities are conducted by groups of people seeking profit through industry, commerce, or agriculture. Commercial activities impacted rivers much more extensively than most activities of pioneer societies. Impacts to water quality, and particularly the U.S. Geological Survey National Water Quality Assessment (NAWQA) program, provide a case study. Results from the 1991–1995 NAWQA program indicate that approximately half the sites sampled in urban areas have surface-water contamination exceeding levels at which adverse biological effects can occur in aquatic biota. Public works such as dam and levee construction undertaken by local and federal governmental agencies caused massive alteration of river systems. Channelization is used as a case study of the impacts of public works on rivers; more than 56,000 km of waterways were channelized by the Corps of Engineers and the Soil Conservation Service after 1940. The net effect of human activities in the United States has been to disconnect rivers from adjacent hillslopes, floodplains, and valley bottoms, underlying hyporheic and groundwater zones, and from headwaters and downstream processes. Because a connected river is a functioning ecosystem, rather than simply a canal for moving water and sediment, disconnection simplifies and impoverishes the ecosystem. This has resulted in widespread loss of biological diversity in rivers of the United States.