Michael John Vepraskas

A rapid approach for ecological assessments in Carolina Bay wetlands that were previously converted to agriculture

FRONTIERS IN FORESTS AND GLOBAL CHANGE, 6.

Phosphorus Fluxes in a Restored Carolina Bay Wetland Following Eight Years of Restoration

WETLANDS, 43(6).

Soil organic carbon changes in a Carolina Bay wetland 15 years after restoration

Moritz, C. M., Vepraskas, M. J., & Ricker, M. C. (2023, March 30). SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, Vol. 3.

Hydrology and Vegetation Relationships in a Carolina Bay Wetland 15 Years after Restoration

WETLANDS, 42(1).

Characterizing copper and zinc content in forested wetland soils of North Carolina, USA

ENVIRONMENTAL MONITORING AND ASSESSMENT, 193(12).

Estimation of Saprolite Thickness Needed to Remove E. coli from Wastewater

APPLIED SCIENCES-BASEL, 11(5).

Development and application of the Hydric Soil Technical Standard

[Review of ]. SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 85(3), 469–487.

Method to Assess Climate Change Impacts on Hydrologic Boundaries of Individual Wetlands

WETLANDS, 40(2), 365–376.

Determining Normal Precipitation Ranges for Hydric Soil Assessments

SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 83(2), 503–510.

Assessing Carolina Bay Wetland Restoration Risks to Downstream Water Quality by Characterizing Land Use and Stream Proximity

Wetlands, 39(3), 495–506.

Citation stacking in soil science articles: our response to the open letter by concerned early-career soil scientists

Geoderma, 328, 119–120.

Phosphorus Dynamics Near Bald Cypress Roots in a Restored Wetland

SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 81(6), 1652–1660.

History of the concept of hydric soil

Wetland Soils: Genesis, Hydrology, Landscapes, and Classification, 2nd Edition, 23–37.

Morphological features of hydric and reduced soils

Wetland Soils: Genesis, Hydrology, Landscapes, and Classification, 2nd Edition, 189–217.

Redox chemistry of hydric soils

Wetland Soils: Genesis, Hydrology, Landscapes, and Classification, 2nd Edition, 105–132.

Using Land-Use Change, Soil Characteristics, and a Semi-Automated On-Line GIS Database to Inventory Carolina Bays

WETLANDS, 37(1), 89–98.

Second edition WETLAND SOILS Genesis, Hydrology, Landscapes, and Classification Preface

Wetland Soils: Genesis, Hydrology, Landscapes, and Classification, 2nd Edition, VII-.

Evaluating Responses of Four Wetland Plant Species to Different Hydroperiods

JOURNAL OF ENVIRONMENTAL QUALITY, 43(2), 723–731.

Phosphorus Dissolution in the Rhizosphere of Bald Cypress Trees in Restored Wetland Soils

SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 79(1), 343–355.

Dissolution of phosphorus into pore-water flowing through an organic soil

GEODERMA, 197, 51–58.

Dynamics of P dissolution processes in the matrix and rhizospheres of bald cypress growing in saturated soil

GEODERMA, 202, 153–160.

Overview of aquic conditions and hydric soils [Chapter 1]

In M. J. Vepraskas & S. W. Sprecher (Eds.), Aquic conditions and hydric soils: The problem soils: Proceedings of a symposium sponsored by Divisions S-10 and S-5 of the Soil Science Society of America and A-2 of the American Society of America [i.e. Agronomy] in Seattle, Washington, 14 November 1994 (pp. 1–22).

Summary [Chapter 9]

In M. J. Vepraskas & S. W. Sprecher (Eds.), Aquic conditions and hydric soils: The problem soils: Proceedings of a symposium sponsored by Divisions S-10 and S-5 of the Soil Science Society of America and A-2 of the American Society of America [i.e. Agronomy] in Seattle, Washington, 14 November 1994 (pp. 153–156).

Differences in Wetland Soil Chemical Soil Properties after 15, 20, and 30 Years of Drainage and Agricultural Production

Geoderma, 179-180, 73–80.

Soil and hydrologic effects on fate and horizontal transport in the capillary fringe of surface-applied nitrate

GEODERMA, 189, 343–350.

Temperature and Water Content Effects on Carbon Mineralization for Sapric Soil Material

Wetlands, 32(5), 939–944.

Linking plant ecology and long-term hydrology to improve wetland restoration success

Transactions of the ASABE, 54(6), 2129–2137.

Surface shading effects on soil C loss in a temperate muck soil

Geoderma, 163(3-4), 238–246.

X-ray Microspectroscopy and Chemical Reactions in Soil Microsites

JOURNAL OF ENVIRONMENTAL QUALITY, 40(3), 667–678.

Plant-Soil-Hydrology Relationships in Three Carolina Bays in Bladen County, North Carolina

CASTANEA, 75(4), 407–420.

Future directions for hydropedology: quantifying impacts of global change on land use

HYDROLOGY AND EARTH SYSTEM SCIENCES, 13(8), 1427–1438.

METHODS TO EVALUATE NORMAL RAINFALL FOR SHORT-TERM WETLAND HYDROLOGY ASSESSMENT

WETLANDS, 29(3), 1049–1062.

Fate of nitrate in the capillary fringe and shallow groundwater in a drained sandy soil

GEODERMA, 146(1-2), 209–215.

Solute transport in the capillary fringe and shallow groundwater: Field evaluation

Vadose Zone Journal, 7(3), 890–898.

Hydropedology of a coarse-loamy catena in the lower Coastal Plain, NC

Severson, E. D., Lindbo, D. L., & Vepraskas, M. J. (2008, April 15). CATENA, Vol. 73, pp. 189–196.

Hydropedology: Fundamental issues and practical applications

Lin, H., Bouma, J., Owens, P., & Vepraskas, M. (2008, April 15). CATENA, Vol. 73, pp. 151–152.

Interpreting morphological features in wetland soils with a hydrologic model

Vepraskas, M. J., & Caldwell, P. V. (2008, April 15). CATENA, Vol. 73, pp. 153–165.

Physical properties of natural organic soils in Carolina Bays of the southeastern United States

SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 71(3), 1051–1057.

Simulating the water budgets of natural Carolina bay wetlands

WETLANDS, 27(4), 1112–1123.

Soil redox potential: Importance, field measurements, and observations

ADVANCES IN AGRONOMY, VOL 94, Vol. 94, pp. 1–54.

Application of ground penetrating radar to aid restoration planning for a drained Carolina Bay

WETLANDS, 26(1), 205–216.

Dynamics of redoximorphic feature formation under controlled ponding in a created riverine wetland

WETLANDS, 26(2), 486–496.

Estimating primary and secondary subsidence in an organic soil 15, 20, and 30 years after drainage

WETLANDS, 26(1), 119–130.

Hydrogeology and pedology of saprolite formed from sedimentary rock, eastern Tennessee, USA

McKay, L. D., Driese, S. G., Smith, K. H., & Vepraskas, M. J. (2005, May). GEODERMA, Vol. 126, pp. 27–45.

Hydrologic models for altered landscapes

Vepraskas, M. J., Huffman, R. L., & Kreiser, G. S. (2006, April). GEODERMA, Vol. 131, pp. 287–298.

Sampling device to extract intact cores in saturated organic soils

SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 69(6), 2071–2075.

Calibrating hydric soil field indicators to long-term wetland hydrology

SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 68(4), 1461–1469.

Predicting contaminant transport along quartz veins above the water table in a mica-schist saprolite

Vepraskas, M. J. (2005, May). GEODERMA, Vol. 126, pp. 47–57.

A method to predict soil saturation frequency and duration from soil color

SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 67(3), 961–969.

Guidelines for analysis and description of soil and regolith thin sections

Adapting a drainage model to simulate water table levels in coastal plain soils

SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 66(5), 1722–1731.

A field method for determing percentage of coated sand grains

SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 65(3), 949–953.

Magnetic susceptibility for use in delineating hydric soils

SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 64(6), 2174–2180.

Morphological changes in soils produced when hydrology is altered by ditching

SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 64(5), 1893–1904.

Physical, chemical and morphological properties of some Regoliths in North Carolina

Southeastern Geology, 39(3/4), 151.

Dynamics of hydric soil formation across the edge of a created deep marsh

WETLANDS, 19(1), 78–89.

Aquic conditions and hydric soils the problem soils : proceedings of a symposium sponsored by Divisions S-10 and S-5 of the Soil Science Society of America and A-2 of the American Society of America [i.e. Agronomy] in Seattle, Washington, 14 November 1994

Biotite alteration to halloysite and kaolinite in soil-saprolite profiles developed from mica schist and granite gneiss

GEODERMA, 75(3-4), 155–170.

IDENTIFYING SOILS WHERE SUBSOILING CAN INCREASE YIELDS OF TOBACCO, CORN, AND COTTON

JOURNAL OF PRODUCTION AGRICULTURE, 5(4), 482–488.

Redoximorphic features for identifying aquic conditions

In Redoximorphic features for identifying aquic conditions (p. 33). Raleigh, NC : North Carolina Agricultural Research Service, North Carolina State University.