Crossref journal-article
Wiley
Limnology and Oceanography (311)
Abstract

In central New Hampshire, sediments of some early Holocene lakes were alkaline and contained carbonate minerals despite granitic bedrock and currently acid soils and surface water in their watersheds. Nearby calcareous bedrock contributed to the till of these watersheds while other lakes, more remote from calcareous bedrock, had early Holocene sediments of neutral pH and devoid of carbonate minerals. Calcite rock fragments in alkaline sediments were eroded from alkaline soils in the watershed. Chemical weathering later acidified these soils and surface waters before modem acid precipitation.

Bibliography

Ryan, D. F., & Kahler, D. M. (1987). Geochemical and mineralogical indications of pH in lakes and soils in central New Hampshire in the early Holocene1. Limnology and Oceanography, 32(3), 751–757. Portico.

Authors 2
  1. Douglas F. Ryan (first)
  2. David M. Kahler (additional)
References 0 Referenced 10

None

Dates
Type When
Created 15 years, 4 months ago (April 7, 2010, 1:54 a.m.)
Deposited 1 year, 10 months ago (Oct. 21, 2023, 12:23 p.m.)
Indexed 1 month, 2 weeks ago (July 4, 2025, 7:48 a.m.)
Issued 38 years, 3 months ago (May 1, 1987)
Published 38 years, 3 months ago (May 1, 1987)
Published Online 21 years, 8 months ago (Dec. 22, 2003)
Published Print 38 years, 3 months ago (May 1, 1987)
Funders 0

None

@article{Ryan_1987, title={Geochemical and mineralogical indications of pH in lakes and soils in central New Hampshire in the early Holocene1}, volume={32}, ISSN={1939-5590}, url={http://dx.doi.org/10.4319/lo.1987.32.3.0751}, DOI={10.4319/lo.1987.32.3.0751}, number={3}, journal={Limnology and Oceanography}, publisher={Wiley}, author={Ryan, Douglas F. and Kahler, David M.}, year={1987}, month=may, pages={751–757} }