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  • Nitrogen cycling, soil properties and infiltration rates along topographic gradient in residential lawns in Baltimore County, Maryland
  • Suchy, Amanda K; City University of New York
    Groffman, Peter M; City University of New York
  • 2020-06-30
  • Suchy, A.K. and P.M. Groffman. 2020. Nitrogen cycling, soil properties and infiltration rates along topographic gradient in residential lawns in Baltimore County, Maryland ver 1. Environmental Data Initiative. https://doi.org/DOI_PLACE_HOLDER (Accessed 2024-12-27).
  • The aim of this research was to examine how topography and homeowner fertilizer practices affected soil and hydrologic properties of residential lawns to determine if there are locations within lawns that have the potential to act as hotspots of nitrogen transport during rain events. This data set contains measurements of saturated infiltration rates, sorptivity, soil moisture, soil organic matter, pH, soil nitrate, soil ammonium, denitrification potentials and limiting factors, and nitrogen mineralization rates from fertilized and unfertilized residential and institutional lawns. Study lawns were located at homes of people who agreed to volunteer their lawn for the study from a door knocking campaign. Four sampling houses were located in an exurban neighborhood in Baisman Run. Five sampling houses were located in a suburban neighborhood in Dead Run. Two sampling locations on institutional lawns were located at University of Maryland Baltimore County. At the exurban study houses and institutional lawns sites,we identified one hillslope to conduct sampling on. At the Dead Run houses we identified one hillslope on the front yard and one in the backyard as there were distinct locations that were not present in the exurban neighborhood. In total we sampled on 16 hillslopes. At each hillslope, we identified the top, toe and swale locations. At each hillslope location, we selected three sampling locations along a transect (maximum 10 meters in length; total of 144 sampling locations). At each sampling location we ran a Cornell Sprinkle Infiltrometer to measure sorptivity and saturated infiltration rates. Volumetric water content was measured before and after infiltrometer runs with a Field Scout TDR 300 with 7.5 cm rods. In addition, at each sampling location we took two soil cores to 10 cm depth, and combined and homogenized the two cores for that sampling location for a total of 144 soil samples. Soil cores were stored on ice in the field, and then stored at 4°C in the lab until processed for variables mentioned above. Sampling for soil cores was conducted in September 2017 with one house collected on 11/1/2017 due to changes in homeowner volunteers. Cornell Sprinkle Infiltrometer measurements were taken in October 2017 with one exception for house DR3. The front yard was conducted on 1/30/2018 and the back yard was completed on 2/27/2018 due to scheduling conflicts and weather interference during October and proceeding months.

  • Geographic Coordinates
    • N: 39.722, S: 39.19, E: -76.33, W: -76.93
    • N: 39.4882, S: 39.46521, E: -76.69033, W: -76.72587
    • N: 39.30473, S: 39.28188, E: -76.72753, W: -76.76155
    • N: 39.26005, S: 39.23346, E: -76.69136, W: -76.72329
  • knb-lter-bes.5006.1  (Uploaded 2020-06-30)  
  • This information is released under the Creative Commons license - Attribution - CC BY (https://creativecommons.org/licenses/by/4.0/). The consumer of these data (\"Data User\" herein) is required to cite it appropriately in any publication that results from its use. The Data User should realize that these data may be actively used by others for ongoing research and that coordination may be necessary to prevent duplicate publication. The Data User is urged to contact the authors of these data if any questions about methodology or results occur. Where appropriate, the Data User is encouraged to consider collaboration or co-authorship with the authors. The Data User should realize that misinterpretation of data may occur if used out of context of the original study. While substantial efforts are made to ensure the accuracy of data and associated documentation, complete accuracy of data sets cannot be guaranteed. All data are made available \"as is.\" The Data User should be aware, however, that data are updated periodically and it is the responsibility of the Data User to check for new versions of the data. The data authors and the repository where these data were obtained shall not be liable for damages resulting from any use or misinterpretation of the data. Thank you.
  • DOI PLACE HOLDER
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