A Reliable U-trough Runoff Collection Method for Quantifying the Migration Loads of Nutrients at Different Soil Layers under Natural Rainfall

Long-term quantification of the migration loads of subsurface runoff (SSR) and its collateral soil nutrients among different soil layers are still restricted by the runoff collection method. This study tested the reliability of the U-trough collection methods (UCM), compared with the seepage plate c...

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Main Authors: Yi Wang, Chengsheng Ni, Sheng Wang, Deti Xie, Jiupai Ni
Format: Article
Language:English
Published: MDPI AG 2021-02-01
Series:Sustainability
Subjects:
UCM
SPM
Online Access:https://www.mdpi.com/2071-1050/13/4/2050
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spelling doaj-48157382438a4c748aa158e928f7bcef2021-02-15T00:01:48ZengMDPI AGSustainability2071-10502021-02-01132050205010.3390/su13042050A Reliable U-trough Runoff Collection Method for Quantifying the Migration Loads of Nutrients at Different Soil Layers under Natural RainfallYi Wang0Chengsheng Ni1Sheng Wang2Deti Xie3Jiupai Ni4College of Resources and Environment, Southwest University, Chongqing 400715, ChinaCollege of Resources and Environment, Southwest University, Chongqing 400715, ChinaCollege of Resources and Environment, Southwest University, Chongqing 400715, ChinaCollege of Resources and Environment, Southwest University, Chongqing 400715, ChinaCollege of Resources and Environment, Southwest University, Chongqing 400715, ChinaLong-term quantification of the migration loads of subsurface runoff (SSR) and its collateral soil nutrients among different soil layers are still restricted by the runoff collection method. This study tested the reliability of the U-trough collection methods (UCM), compared with the seepage plate collection method (SPM), in monitoring the runoff, sediment and nutrient migration loads from different soil layers (L<sub>1</sub>: 0–20 cm depth; L<sub>2</sub>: 20–40 cm depth; L<sub>3</sub>: 40–60 cm depth) for two calendar years under natural rainfall events. The results suggested that the U-trough could collect nearly 10 times the SSR sample volume of the seepage plate and keep the sampling probability more than 95% at each soil layer. The annual SSR flux from L<sub>1</sub> to L<sub>3</sub> was 403.4 mm, 271.9 mm, and 237.4 mm under the UCM, 14.35%, 10.56%, and 8.41% lower than those under the SPM, respectively. The annual net migration loads of sediment, TN, and TP from the L<sub>1</sub> layer under the UCM were 49.562 t/km<sup>2</sup>, 19.113 t/km<sup>2</sup> and 0.291 t/km<sup>2</sup>, and 86.62%, 41.21% and 81.78% of them were intercepted by the subsoil layers (L<sub>2</sub> and L<sub>3</sub>), respectively. While their migration loads under the SPM were 48.708 t/km<sup>2</sup>, 22.342 t/km<sup>2</sup> and 0.291 t/km<sup>2</sup>, and 88.24%, 53.06% and 80.42% of them were intercepted, respectively. Under both methods, the average leached total <i>n</i> (TN), total <i>p</i> (TP) concentrations per rainfall event and their annual migrated loads at each soil layer showed no significant difference. In conclusion, the UCM was a reliable quantitative method for subsurface runoff, sediment, and soil nutrient migration loads from diverse soil layers of purple soil sloping cultivated lands. Further studies are needed to testify the availability in other lands.https://www.mdpi.com/2071-1050/13/4/2050UCMSPMstratified quantitative researchnitrogen migration loadphosphorus migration load
collection DOAJ
language English
format Article
sources DOAJ
author Yi Wang
Chengsheng Ni
Sheng Wang
Deti Xie
Jiupai Ni
spellingShingle Yi Wang
Chengsheng Ni
Sheng Wang
Deti Xie
Jiupai Ni
A Reliable U-trough Runoff Collection Method for Quantifying the Migration Loads of Nutrients at Different Soil Layers under Natural Rainfall
Sustainability
UCM
SPM
stratified quantitative research
nitrogen migration load
phosphorus migration load
author_facet Yi Wang
Chengsheng Ni
Sheng Wang
Deti Xie
Jiupai Ni
author_sort Yi Wang
title A Reliable U-trough Runoff Collection Method for Quantifying the Migration Loads of Nutrients at Different Soil Layers under Natural Rainfall
title_short A Reliable U-trough Runoff Collection Method for Quantifying the Migration Loads of Nutrients at Different Soil Layers under Natural Rainfall
title_full A Reliable U-trough Runoff Collection Method for Quantifying the Migration Loads of Nutrients at Different Soil Layers under Natural Rainfall
title_fullStr A Reliable U-trough Runoff Collection Method for Quantifying the Migration Loads of Nutrients at Different Soil Layers under Natural Rainfall
title_full_unstemmed A Reliable U-trough Runoff Collection Method for Quantifying the Migration Loads of Nutrients at Different Soil Layers under Natural Rainfall
title_sort reliable u-trough runoff collection method for quantifying the migration loads of nutrients at different soil layers under natural rainfall
publisher MDPI AG
series Sustainability
issn 2071-1050
publishDate 2021-02-01
description Long-term quantification of the migration loads of subsurface runoff (SSR) and its collateral soil nutrients among different soil layers are still restricted by the runoff collection method. This study tested the reliability of the U-trough collection methods (UCM), compared with the seepage plate collection method (SPM), in monitoring the runoff, sediment and nutrient migration loads from different soil layers (L<sub>1</sub>: 0–20 cm depth; L<sub>2</sub>: 20–40 cm depth; L<sub>3</sub>: 40–60 cm depth) for two calendar years under natural rainfall events. The results suggested that the U-trough could collect nearly 10 times the SSR sample volume of the seepage plate and keep the sampling probability more than 95% at each soil layer. The annual SSR flux from L<sub>1</sub> to L<sub>3</sub> was 403.4 mm, 271.9 mm, and 237.4 mm under the UCM, 14.35%, 10.56%, and 8.41% lower than those under the SPM, respectively. The annual net migration loads of sediment, TN, and TP from the L<sub>1</sub> layer under the UCM were 49.562 t/km<sup>2</sup>, 19.113 t/km<sup>2</sup> and 0.291 t/km<sup>2</sup>, and 86.62%, 41.21% and 81.78% of them were intercepted by the subsoil layers (L<sub>2</sub> and L<sub>3</sub>), respectively. While their migration loads under the SPM were 48.708 t/km<sup>2</sup>, 22.342 t/km<sup>2</sup> and 0.291 t/km<sup>2</sup>, and 88.24%, 53.06% and 80.42% of them were intercepted, respectively. Under both methods, the average leached total <i>n</i> (TN), total <i>p</i> (TP) concentrations per rainfall event and their annual migrated loads at each soil layer showed no significant difference. In conclusion, the UCM was a reliable quantitative method for subsurface runoff, sediment, and soil nutrient migration loads from diverse soil layers of purple soil sloping cultivated lands. Further studies are needed to testify the availability in other lands.
topic UCM
SPM
stratified quantitative research
nitrogen migration load
phosphorus migration load
url https://www.mdpi.com/2071-1050/13/4/2050
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