Reclamation of Acid Sulfate Soils Using Lime-Stabilized Biosolids
Excavation of sulfidic materials during construction has resulted in acid rock drainage (ARD) problems throughout Virginia. The most extensive documented uncontrolled disturbance at a single location is Stafford Regional Airport (SRAP) in Stafford, Virginia. Beginning in 1998, over 150 ha of sulfidi...
Saved in:
Published in | Journal of environmental quality Vol. 37; no. 4; pp. 1447 - 1455 |
---|---|
Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Madison
American Society of Agronomy, Crop Science Society of America, Soil Science Society
01.07.2008
American Society of Agronomy |
Subjects | |
Online Access | Get full text |
Cover
Loading…
Summary: | Excavation of sulfidic materials during construction has resulted in acid rock drainage (ARD) problems throughout Virginia. The most extensive documented uncontrolled disturbance at a single location is Stafford Regional Airport (SRAP) in Stafford, Virginia. Beginning in 1998, over 150 ha of sulfidic Coastal Plain sediments were disturbed, including steeply sloping cut surfaces and spoils placed into fills. Acid sulfate soils developed, and ARD generated on-site degraded metal and concrete structures and heavily damaged water quality with effects noted over 1 km downstream. The site was not recognized as sulfidic until 2001 when surface soil sampling revealed pH values ranging from 1.9 to 5.3 and peroxide potential acidity (PPA) values ranging from 1 to 42 Mg CaCO3 per 1000 Mg material. In February 2002 a water quality program was established in and around the site to monitor baseline pH, EC, NO3-N, NH4-N, PO4-P, Fe, Al, Mn, and SO4-S, and initial pH values as low as 2.9 were noted in on-site receiving streams. In the spring and fall of 2002, the site was treated with variable rates of lime-stabilized biosolids, straw-mulch, and acid- and salt-tolerant legumes and grasses. By October 2002, the site was fully revegetated (> or = 90% living cover) with the exception of a few highly acidic outcrops and seepage areas. Surface soil sampling in 2003, 2004, and 2006 revealed pH values typically > 6.0. Water quality responded quickly to treatment, although short-term NH4+ release occurred. Despite heavy loadings, no significant surface water P losses were observed. |
---|---|
Bibliography: | http://dx.doi.org/10.2134/jeq2007.0206 All rights reserved. No part of this periodical may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage and retrieval system, without permission in writing from the publisher. ObjectType-Article-2 SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 14 content type line 23 ObjectType-Article-1 ObjectType-Feature-2 |
ISSN: | 0047-2425 1537-2537 1537-2537 |
DOI: | 10.2134/jeq2007.0206 |