|
North Dakota Water Resources Research Institute
|
|
Title:
Wetland Hydrology of Minelands in West
Central North Dakota Focus Categories: Wetlands, Hydrology Project
No.
ND93-04 Principal
Investigators
Completion Report Sharma,
P.P. and J.L. Richardson, 1996, Wetland Hydrology of Minelands in West Central
North Dakota, Rept. No. ND-93-04, North Dakota Water Resources Research
Institute, North Dakota State University, Fargo, 87 pages. Publications Sharma,
P. P., F. S. Carter, B. J. Baker, and J. L. Richardson. 1995. Hydrology of
prairie wetlands in surface coal minelands of North Dakota.
Journal of the Minnesota Academy of Science,
59, 6 pages. Baker,
Barbara J., 1996. Soil Formation of Wetlands in Abandoned Mine Lands of North
Dakota. “M.S. Thesis”, Department of Soil Science, North Dakota State
University, Fargo, 91 pages. Sharma,
P.P. 1995. Hydrologic
characterization of wetlands in surface coal minelands of North Dakota.
Proceedings of the annual Meeting of the American Society for Surface Mining and
Reclamation, Gillette, Wyoming, June 5‑8. pp. 839. Sharma,
P. P., F. S. Carter and J. Solc. 1996. Hydrologic characteristics of natural and
reconstructed prairie wetlands, in Proceedings of the Fifth Biennial North
Dakota Water Quality Symposium, B.D. Seelig, ed. NDSU Extension Service, pp.
22-23. Sharma,
P.P. and J.L. Richardson, 1993, Wetland hydrology of minelands: A research
initiative, in
1993 Proceedings of Mineland Reclamation Research Review, Land
Reclamation Research
Center and Northern Great Plains Research Center, March 15, Mandan, ND,
pp. 59‑65. The
study led to an improved understanding of wetland functions in natural and
constructed wetlands in the minelands in Central North Dakota. The wetland ponds
used in the study were recharge wetlands, exclusively, with very low dissolved
salt content. The fact that one of the wetlands is a permanent pond suggested
that in the saline and sodic orphan spoil landscapes, runoff occurs rapidly with
little infiltration. These wetlands do not appear to receive ground water from
any sources. In nearby rangeland, runoff water is not common. The soil
development represents the recharge conditions. The edges have more development
than the wetland centers. |
|
Return to ND WRRI Home Page |