Initial aggregate formation and soil carbon storage from lipid-extracted algae amendment

Soil organic C (SOC) storage results when organic matter inputs to soil exceed losses through decomposition, and is strongly influenced by organic matter effects on soil aggregation. We evaluated the initial effects of lipid-extracted algae (LEA), a byproduct of biofuel production, on soil aggregate...

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Main Authors: Katie Lewis, Jamie Foster, Frank Hons, Thomas Boutton
Format: Article
Language:English
Published: AIMS Press 2017-12-01
Series:AIMS Environmental Science
Subjects:
Online Access:http://www.aimspress.com/environmental/article/1735/fulltext.html
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spelling doaj-951344ce20c74dcb970d437e17d154de2020-11-25T02:10:27ZengAIMS PressAIMS Environmental Science2372-03522017-12-014674376210.3934/environsci.2017.6.743environ-04-00743Initial aggregate formation and soil carbon storage from lipid-extracted algae amendmentKatie Lewis0Jamie Foster1Frank Hons2Thomas Boutton3Texas A&amp;M AgriLife Research, Texas A&amp;M University, Lubbock, TX, USATexas A&amp;M AgriLife Research, Texas A&amp;M University, Beeville, TX, USASoil and Crop Sciences Department, Texas A&amp;M University, College Station, TX, USAEcosystem Science Management Department, Texas A&amp;M University, College Station, TX, USASoil organic C (SOC) storage results when organic matter inputs to soil exceed losses through decomposition, and is strongly influenced by organic matter effects on soil aggregation. We evaluated the initial effects of lipid-extracted algae (LEA), a byproduct of biofuel production, on soil aggregate formation and SOC storage. In situ field incubations were conducted by amending soil with (1) 1.5% LEA, (2) 3.0% LEA, (3) 1.5% LEA + 1.5% wheat straw (WS) and (4) soil plus inorganic N (140 kg ha<sup>−1</sup> NH<sub>4</sub>NO<sub>3</sub>) and P [112 kg ha<sup>−1</sup> Ca(H<sub>2</sub>PO<sub>4</sub>)<sub>2</sub>·H<sub>2</sub>O] as the control. Soil samples were collected 0, 3, 6, 9, and 12 months after treatment application at 0–5, 5–15, and 15–30 cm. Soil was separated into macroaggregate (&gt;250 µm), microaggregate (250–53 µm), and silt and clay (&lt;53 µm) fractions by dry-sieving, and mean weight diameter was calculated. Soils and soil fractions were analyzed to determine C concentrations and associated δ<sup>13</sup>C values. Mean weight diameter 12 months after 3.0% LEA application was greater than the 1.5% LEA + 1.5% WS addition at the 5–15 cm depth. Soil amended with 1.5% LEA, 3.0% LEA or 1.5% LEA + 1.5% WS resulted in greater SOC after 12 months for all soil size fractions and depths. δ<sup>13</sup>C indicated that most LEA-C was initially associated with the silt and clay fraction, but later became more strongly associated with the macro- and microaggregate fractions after 12 months. Soil application of LEA enhanced initial aggregate formation and SOC storage by increasing aggregate MWD and macro- and microaggregate associated SOC over time. As the world population grows and resources become more limited, use of alternative energy sources, soil conservation, and environmental protection must be top research priorities. Our research emphasized all three and demonstrated that LEA can enhance soil structure and C storage.http://www.aimspress.com/environmental/article/1735/fulltext.htmlsoil organic carboncarbon storageaggregate stabilitysoil amendmentalgal residuebioenergy feedstockwheat straw residueorganic mattersoil structurestable carbon isotopic composition
collection DOAJ
language English
format Article
sources DOAJ
author Katie Lewis
Jamie Foster
Frank Hons
Thomas Boutton
spellingShingle Katie Lewis
Jamie Foster
Frank Hons
Thomas Boutton
Initial aggregate formation and soil carbon storage from lipid-extracted algae amendment
AIMS Environmental Science
soil organic carbon
carbon storage
aggregate stability
soil amendment
algal residue
bioenergy feedstock
wheat straw residue
organic matter
soil structure
stable carbon isotopic composition
author_facet Katie Lewis
Jamie Foster
Frank Hons
Thomas Boutton
author_sort Katie Lewis
title Initial aggregate formation and soil carbon storage from lipid-extracted algae amendment
title_short Initial aggregate formation and soil carbon storage from lipid-extracted algae amendment
title_full Initial aggregate formation and soil carbon storage from lipid-extracted algae amendment
title_fullStr Initial aggregate formation and soil carbon storage from lipid-extracted algae amendment
title_full_unstemmed Initial aggregate formation and soil carbon storage from lipid-extracted algae amendment
title_sort initial aggregate formation and soil carbon storage from lipid-extracted algae amendment
publisher AIMS Press
series AIMS Environmental Science
issn 2372-0352
publishDate 2017-12-01
description Soil organic C (SOC) storage results when organic matter inputs to soil exceed losses through decomposition, and is strongly influenced by organic matter effects on soil aggregation. We evaluated the initial effects of lipid-extracted algae (LEA), a byproduct of biofuel production, on soil aggregate formation and SOC storage. In situ field incubations were conducted by amending soil with (1) 1.5% LEA, (2) 3.0% LEA, (3) 1.5% LEA + 1.5% wheat straw (WS) and (4) soil plus inorganic N (140 kg ha<sup>−1</sup> NH<sub>4</sub>NO<sub>3</sub>) and P [112 kg ha<sup>−1</sup> Ca(H<sub>2</sub>PO<sub>4</sub>)<sub>2</sub>·H<sub>2</sub>O] as the control. Soil samples were collected 0, 3, 6, 9, and 12 months after treatment application at 0–5, 5–15, and 15–30 cm. Soil was separated into macroaggregate (&gt;250 µm), microaggregate (250–53 µm), and silt and clay (&lt;53 µm) fractions by dry-sieving, and mean weight diameter was calculated. Soils and soil fractions were analyzed to determine C concentrations and associated δ<sup>13</sup>C values. Mean weight diameter 12 months after 3.0% LEA application was greater than the 1.5% LEA + 1.5% WS addition at the 5–15 cm depth. Soil amended with 1.5% LEA, 3.0% LEA or 1.5% LEA + 1.5% WS resulted in greater SOC after 12 months for all soil size fractions and depths. δ<sup>13</sup>C indicated that most LEA-C was initially associated with the silt and clay fraction, but later became more strongly associated with the macro- and microaggregate fractions after 12 months. Soil application of LEA enhanced initial aggregate formation and SOC storage by increasing aggregate MWD and macro- and microaggregate associated SOC over time. As the world population grows and resources become more limited, use of alternative energy sources, soil conservation, and environmental protection must be top research priorities. Our research emphasized all three and demonstrated that LEA can enhance soil structure and C storage.
topic soil organic carbon
carbon storage
aggregate stability
soil amendment
algal residue
bioenergy feedstock
wheat straw residue
organic matter
soil structure
stable carbon isotopic composition
url http://www.aimspress.com/environmental/article/1735/fulltext.html
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