
Position of transects shown in red. Not to scale
Soil transects were taken in August 1993 across the boundaries between four pairs of adjacent unlimed 'd' sub-plots with different fertiliser treatments on the Park Grass experiment, to assess the extent to which fertiliser in one plot affects the soil of the adjacent plot. All the soils were analysed for pH (in water); the soil from two pairs of plots were also analysed for Olsen P and exchangeable cations. The data shows that there has been some mixing across the plot boundaries, possibly because, over 137 years (when the samples were taken) some fertiliser may not have been applied right up to the plot boundary or might have been spread over the boundary. It also seems likely that plant roots would have spread into adjacent plots looking for nutrients; the roots subsequently die leaving slightly enriched residues in the soil. However, in all cases, soil from > 50 cm away from the boundary is less variable. This is the data discussed in Poulton et al, 2026 (in preparation).
Two transects (50 and 100 cm from the plot edge) were taken across the boundaries between four pairs of adjacent plots (14-2d and 1d, 1d and 2d, 4-1d and 4-2d, 11-2d and 12d) which had very contrasting fertiliser treatments, on 13th August 1993. Soil cores (0-23 cm depth) were taken at 0, 10, 20, 30, 40, 50, 65, 80, 100, 125, 150, 175, 200, 250, 300, 350, 400, 450 and 500 cm from the shared plot boundary, a total of 19 samples from each transect from each plot. The common boundary between each plot pair is indicated by distance zero and sample 1. All pairs of plots share the same sample for distance zero, except pairs 1d and 2d, where the transects were not contiguous (see figure). In the dataset negative distances from the boundary indicate samples taken on the east side of the common boundary, positive distances indicate samples taken on the west side of the common boundary, to aid plotting the data.
Soil properties:
Soil cores from the same point on each of the duplicate transects were bulked, dried and ground < 2 mm and analysed.
Soil pH in boiled, deionised water
Soil Olsen P, a measure of plant-available soil P. Measured after extraction with 0.5M NaHCO3 (Olsen, 1954) using a modified method of Murphy and Riley (1962) on a continuous segmented colourimetric flow analyser (Skalar SANPLUS, Skalar Analytical BV, Breda, Netherlands).
Soil exchangeable cations: potassium (K), calcium (Ca), magnesium (Mg), sodium (Na), aluminium (Al) and iron (Fe) leached with 1M ammonium acetate (Metson, 1956) and determined by ICP-OES (Inductively Coupled Plasma - Optical Emission Spectrometry), (Agilent 5900 SVDV ICP-OES, Agilent Technologies 5301 Stevens Creek Blvd. Santa Clara, CA 95051, USA).
Rothamsted Research
This
dataset is
available under a Creative
Commons
Attribution Licence (4.0).
YOU MUST CITE AS: Poulton, P., Glendining, M. (2025). Dataset: Park Grass 1993 soil transects across adjacent pairs of sub-plots with contrasting treatments Electronic Rothamsted Archive, Rothamsted Research, Harpenden, UK https://doi.org/10.23637/rpg5-transects-01
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An Excel file, rpg5_transects_01.xlsx, contains Park Grass transect data for 1993. Frictionless CSV files are also provided.
This dataset is from measurements made by Paul Poulton, and analysed by the Analytical Chemistry Unit, Rothamsted Research, Harpenden.
The Analytical Chemistry Unit follows the Joint Code of Practice (JCoPR) and participates in European Quality Assurance programmes. All performance is strictly monitored using certified external standards alongside in-house standard materials. Standards and check samples are monitored and recorded.
References for methods of analysis:
For further information and assistance, please contact the e-RA curators, Sarah Perryman and Margaret Glendining using the e-RA email address: era@rothamsted.ac.uk