Geostatistical Determination of Soil Noise and Soil Phosphorus Spatial Variability

This research studies the effect of stratifying soil samples to try and find a suitable depth to establish a geospatial relationship for a practical soil sampling grid in New Zealand hill country. Cores were collected from 200 predetermined sites in grids at two trial sites at “Patitapu” hill countr...

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Main Authors: Therese Kaul, Miles Grafton
Format: Article
Language:English
Published: MDPI AG 2017-09-01
Series:Agriculture
Subjects:
Online Access:https://www.mdpi.com/2077-0472/7/10/83
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spelling doaj-da37a59af3f544c0babd702effff3bbe2021-04-02T05:49:10ZengMDPI AGAgriculture2077-04722017-09-017108310.3390/agriculture7100083agriculture7100083Geostatistical Determination of Soil Noise and Soil Phosphorus Spatial VariabilityTherese Kaul0Miles Grafton1Institute of Agriculture and Environment, Massey University, Private Bag, Palmerston North 4474, New ZealandInstitute of Agriculture and Environment, Massey University, Private Bag, Palmerston North 4474, New ZealandThis research studies the effect of stratifying soil samples to try and find a suitable depth to establish a geospatial relationship for a practical soil sampling grid in New Zealand hill country. Cores were collected from 200 predetermined sites in grids at two trial sites at “Patitapu” hill country farm in the Wairarapa, New Zealand. Trial 1 was a 200 m × 100 m grid located in a gently undulating paddock. Trial 2 was a 220 m × 80 m grid located on a moderately sloped paddock. Each grid had cores taken at intervals of 5 m, 10 m, or 20 m. Core sites were mapped out prior to going into the field; these points were found using a Leica Geo Systems GS15 (real time kinematic GPS) and marked with pigtail pegs and spray-paint on the ground. Cores were taken using a 50 mm-diameter soil core sampler. Cores were cut into three sections according to depth: A—0–30 mm, B—30–75 mm, and C—75–150 mm. Olsen P lab results were obtained for half of the total 1400 samples due to financial constraints. The results indicate that there was a significant decrease in variability from Section A to Section B for both trials. Section B and C for Trial 1 had similar variability, whereas there was another significant drop in variability from Section B to C in Trial 2. Measuring samples below the top 3 cm appeared to effectively reduce noise when sampled from 3 to 15 cm. However, measuring from 7.5 cm to 15 cm on the slope in Trial 2 reduced variability so much that all results were almost identical, which may mean that there is no measurable representation of plant available P. The reduction in noise by removing the top 3 cm of soil samples is significant for improving current soil nutrient testing methods by allowing better geospatial predictions for whole paddock soil nutrient variability mapping.https://www.mdpi.com/2077-0472/7/10/83soil phosphorusgeo-statisticsspatial variabilityOlsen Pstatistical noise
collection DOAJ
language English
format Article
sources DOAJ
author Therese Kaul
Miles Grafton
spellingShingle Therese Kaul
Miles Grafton
Geostatistical Determination of Soil Noise and Soil Phosphorus Spatial Variability
Agriculture
soil phosphorus
geo-statistics
spatial variability
Olsen P
statistical noise
author_facet Therese Kaul
Miles Grafton
author_sort Therese Kaul
title Geostatistical Determination of Soil Noise and Soil Phosphorus Spatial Variability
title_short Geostatistical Determination of Soil Noise and Soil Phosphorus Spatial Variability
title_full Geostatistical Determination of Soil Noise and Soil Phosphorus Spatial Variability
title_fullStr Geostatistical Determination of Soil Noise and Soil Phosphorus Spatial Variability
title_full_unstemmed Geostatistical Determination of Soil Noise and Soil Phosphorus Spatial Variability
title_sort geostatistical determination of soil noise and soil phosphorus spatial variability
publisher MDPI AG
series Agriculture
issn 2077-0472
publishDate 2017-09-01
description This research studies the effect of stratifying soil samples to try and find a suitable depth to establish a geospatial relationship for a practical soil sampling grid in New Zealand hill country. Cores were collected from 200 predetermined sites in grids at two trial sites at “Patitapu” hill country farm in the Wairarapa, New Zealand. Trial 1 was a 200 m × 100 m grid located in a gently undulating paddock. Trial 2 was a 220 m × 80 m grid located on a moderately sloped paddock. Each grid had cores taken at intervals of 5 m, 10 m, or 20 m. Core sites were mapped out prior to going into the field; these points were found using a Leica Geo Systems GS15 (real time kinematic GPS) and marked with pigtail pegs and spray-paint on the ground. Cores were taken using a 50 mm-diameter soil core sampler. Cores were cut into three sections according to depth: A—0–30 mm, B—30–75 mm, and C—75–150 mm. Olsen P lab results were obtained for half of the total 1400 samples due to financial constraints. The results indicate that there was a significant decrease in variability from Section A to Section B for both trials. Section B and C for Trial 1 had similar variability, whereas there was another significant drop in variability from Section B to C in Trial 2. Measuring samples below the top 3 cm appeared to effectively reduce noise when sampled from 3 to 15 cm. However, measuring from 7.5 cm to 15 cm on the slope in Trial 2 reduced variability so much that all results were almost identical, which may mean that there is no measurable representation of plant available P. The reduction in noise by removing the top 3 cm of soil samples is significant for improving current soil nutrient testing methods by allowing better geospatial predictions for whole paddock soil nutrient variability mapping.
topic soil phosphorus
geo-statistics
spatial variability
Olsen P
statistical noise
url https://www.mdpi.com/2077-0472/7/10/83
work_keys_str_mv AT theresekaul geostatisticaldeterminationofsoilnoiseandsoilphosphorusspatialvariability
AT milesgrafton geostatisticaldeterminationofsoilnoiseandsoilphosphorusspatialvariability
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