1970
DOI: 10.3133/ofr70274
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A hydrologic analysis of the New Jersey Pine Barrens region

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Cited by 17 publications
(15 citation statements)
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“…This unit, the Cohansey Formation, is a wedge of unconsolidated sands and gravels of Tertiary age, 45-75 m in thickness near the Atlantic Coast and becoming less thick to the west (Rhodehamel, 1979). In the highly permeable sand, water infiltrates rapidly, so that the soil surface in the uplands is usually arid (Rhodehamel, 1970).…”
Section: Clinal Variation In Fire Frequencymentioning
confidence: 99%
“…This unit, the Cohansey Formation, is a wedge of unconsolidated sands and gravels of Tertiary age, 45-75 m in thickness near the Atlantic Coast and becoming less thick to the west (Rhodehamel, 1979). In the highly permeable sand, water infiltrates rapidly, so that the soil surface in the uplands is usually arid (Rhodehamel, 1970).…”
Section: Clinal Variation In Fire Frequencymentioning
confidence: 99%
“…Upward seepage gradients have been reported within the Cohansey-Kirkwood Formation (Rhodehamel, 1970) and the idealized flow system shown I in Figure 3-10 has been suggested. In this diagram, the BOMARC Missile Site would fall within the outer fringes of the upland recharge area, where local recharge of the shallow portions of the aquifer is favored, and the depth of penetration of this recharge water is limited.…”
Section: Groundwater Flow Characteristicsmentioning
confidence: 99%
“…The hydraulic conductivity ranges from 750 to 1,000 gallons per day (gpd) per square foot, typical of well-sorted sands and gravels. The transmissivity ranges from 75,000 to 100,000 gpd per foot and the specific yield generally is less than 25 percent, typical of fine gravel to gravely sand (Rhodehamel, 1970).…”
mentioning
confidence: 99%
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“…Other relevant works that pertain to the ecology and related hydrology of the Kirkwood-Cohansey aquifer system in the Pinelands include reports by Bunnell and Ciraolo (2010), Kennen and Riskin (2010), Laidig (2010), Laidig andothers (2009, 2010), Lathrop and others (2010), Procopio (2010), Zampella and others (1992Zampella and others ( , 2001aZampella and others ( , 2001bZampella and others ( , 2003 2008), and Yu and Ehrenfeld (2009); a study of Pinelands vegetation by McCormick (1979); reports on the hydrology of and water resources in the Pinelands area (Rhodehamel, 1970(Rhodehamel, , 1973(Rhodehamel, , 1979; a study of evaporation from wetlands by Buell and Ballard (1972), and a report on insects, fire, and ET in the Pinelands by Clark and others (2012). Reports by Lord and others (1990) and Johnsson and Barringer (1993) present results of a water-quality and hydrologic study of the McDonalds Branch Basin.…”
Section: Related Studies and Previous Investigationsmentioning
confidence: 99%