Changes of oxygen isotope values of soil P pools associated with changes in soil pH
Field data about the effect of soil pH on phosphorus (P) cycling is limited. A promising tool to study P cycling under field conditions is the 18 O: 16 O ratio of phosphate (δ 18 O P ). In this study we investigate whether the δ 18 O P can be used to elucidate the effect of soil pH on P cycling in g...
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| Published in | Scientific reports Vol. 10; no. 1; p. 2065 |
|---|---|
| Main Authors | , , , , , , |
| Format | Journal Article |
| Language | English |
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Nature Publishing Group UK
07.02.2020
Nature Publishing Group |
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| Abstract | Field data about the effect of soil pH on phosphorus (P) cycling is limited. A promising tool to study P cycling under field conditions is the
18
O:
16
O ratio of phosphate (δ
18
O
P
). In this study we investigate whether the δ
18
O
P
can be used to elucidate the effect of soil pH on P cycling in grasslands. Soils and plants were sampled from different fertilisation and lime treatments of the Park Grass long term experiment at Rothamsted Research, UK. The soils were sequentially extracted to isolate different soil P pools, including available P and corresponding δ
18
O
P
values were determined. We did not observe changes in plant δ
18
O
P
value, but soil P δ
18
O
P
values changed, and lower δ
18
O
P
values were associated with higher soil pH values. At sites where P was not limiting, available P δ
18
O
P
increased by up to 3‰ when lime was applied. We show that the δ
18
O
P
method is a useful tool to investigate the effect of pH on soil P cycling under field conditions as it highlights that different soil processes must govern P availability as pH shifts. The next challenge is now to identify these underlying processes, enabling better management of soil P at different pH. |
|---|---|
| AbstractList | Field data about the effect of soil pH on phosphorus (P) cycling is limited. A promising tool to study P cycling under field conditions is the 18O:16O ratio of phosphate (δ18OP). In this study we investigate whether the δ18OP can be used to elucidate the effect of soil pH on P cycling in grasslands. Soils and plants were sampled from different fertilisation and lime treatments of the Park Grass long term experiment at Rothamsted Research, UK. The soils were sequentially extracted to isolate different soil P pools, including available P and corresponding δ18OP values were determined. We did not observe changes in plant δ18OP value, but soil P δ18OP values changed, and lower δ18OP values were associated with higher soil pH values. At sites where P was not limiting, available P δ18OP increased by up to 3‰ when lime was applied. We show that the δ18OP method is a useful tool to investigate the effect of pH on soil P cycling under field conditions as it highlights that different soil processes must govern P availability as pH shifts. The next challenge is now to identify these underlying processes, enabling better management of soil P at different pH. Field data about the effect of soil pH on phosphorus (P) cycling is limited. A promising tool to study P cycling under field conditions is the 18 O: 16 O ratio of phosphate (δ 18 O P ). In this study we investigate whether the δ 18 O P can be used to elucidate the effect of soil pH on P cycling in grasslands. Soils and plants were sampled from different fertilisation and lime treatments of the Park Grass long term experiment at Rothamsted Research, UK. The soils were sequentially extracted to isolate different soil P pools, including available P and corresponding δ 18 O P values were determined. We did not observe changes in plant δ 18 O P value, but soil P δ 18 O P values changed, and lower δ 18 O P values were associated with higher soil pH values. At sites where P was not limiting, available P δ 18 O P increased by up to 3‰ when lime was applied. We show that the δ 18 O P method is a useful tool to investigate the effect of pH on soil P cycling under field conditions as it highlights that different soil processes must govern P availability as pH shifts. The next challenge is now to identify these underlying processes, enabling better management of soil P at different pH. Field data about the effect of soil pH on phosphorus (P) cycling is limited. A promising tool to study P cycling under field conditions is the 18O:16O ratio of phosphate (δ18OP). In this study we investigate whether the δ18OP can be used to elucidate the effect of soil pH on P cycling in grasslands. Soils and plants were sampled from different fertilisation and lime treatments of the Park Grass long term experiment at Rothamsted Research, UK. The soils were sequentially extracted to isolate different soil P pools, including available P and corresponding δ18OP values were determined. We did not observe changes in plant δ18OP value, but soil P δ18OP values changed, and lower δ18OP values were associated with higher soil pH values. At sites where P was not limiting, available P δ18OP increased by up to 3‰ when lime was applied. We show that the δ18OP method is a useful tool to investigate the effect of pH on soil P cycling under field conditions as it highlights that different soil processes must govern P availability as pH shifts. The next challenge is now to identify these underlying processes, enabling better management of soil P at different pH.Field data about the effect of soil pH on phosphorus (P) cycling is limited. A promising tool to study P cycling under field conditions is the 18O:16O ratio of phosphate (δ18OP). In this study we investigate whether the δ18OP can be used to elucidate the effect of soil pH on P cycling in grasslands. Soils and plants were sampled from different fertilisation and lime treatments of the Park Grass long term experiment at Rothamsted Research, UK. The soils were sequentially extracted to isolate different soil P pools, including available P and corresponding δ18OP values were determined. We did not observe changes in plant δ18OP value, but soil P δ18OP values changed, and lower δ18OP values were associated with higher soil pH values. At sites where P was not limiting, available P δ18OP increased by up to 3‰ when lime was applied. We show that the δ18OP method is a useful tool to investigate the effect of pH on soil P cycling under field conditions as it highlights that different soil processes must govern P availability as pH shifts. The next challenge is now to identify these underlying processes, enabling better management of soil P at different pH. Field data about the effect of soil pH on phosphorus (P) cycling is limited. A promising tool to study P cycling under field conditions is the O: O ratio of phosphate (δ O ). In this study we investigate whether the δ O can be used to elucidate the effect of soil pH on P cycling in grasslands. Soils and plants were sampled from different fertilisation and lime treatments of the Park Grass long term experiment at Rothamsted Research, UK. The soils were sequentially extracted to isolate different soil P pools, including available P and corresponding δ O values were determined. We did not observe changes in plant δ O value, but soil P δ O values changed, and lower δ O values were associated with higher soil pH values. At sites where P was not limiting, available P δ O increased by up to 3‰ when lime was applied. We show that the δ O method is a useful tool to investigate the effect of pH on soil P cycling under field conditions as it highlights that different soil processes must govern P availability as pH shifts. The next challenge is now to identify these underlying processes, enabling better management of soil P at different pH. |
| ArticleNumber | 2065 |
| Author | Granger, Steven J. Blackwell, Martin S. A. Smith, Andrew C. Mead, Andrew Pfahler, Verena Tamburini, Federica Macdonald, Andy |
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| BackLink | https://www.ncbi.nlm.nih.gov/pubmed/32034236$$D View this record in MEDLINE/PubMed |
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| CitedBy_id | crossref_primary_10_1016_j_apgeochem_2021_104978 crossref_primary_10_1002_jpln_202000378 crossref_primary_10_1016_j_catena_2024_108572 crossref_primary_10_1007_s11676_022_01582_2 crossref_primary_10_1016_j_quascirev_2024_109028 |
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| Snippet | Field data about the effect of soil pH on phosphorus (P) cycling is limited. A promising tool to study P cycling under field conditions is the
18
O:
16
O ratio... Field data about the effect of soil pH on phosphorus (P) cycling is limited. A promising tool to study P cycling under field conditions is the O: O ratio of... Field data about the effect of soil pH on phosphorus (P) cycling is limited. A promising tool to study P cycling under field conditions is the 18O:16O ratio of... |
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| Title | Changes of oxygen isotope values of soil P pools associated with changes in soil pH |
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