Register      Login
Soil Research Soil Research Society
Soil, land care and environmental research
RESEARCH ARTICLE

Labile soil carbon fractions as indicators of soil quality improvement under short-term grassland set-aside

Jason M. Lussier A , Maja Krzic https://orcid.org/0000-0003-3919-3252 A B C , Sean M. Smukler A , Katarina R. Neufeld A , Chantel J. Chizen A and Art A. Bomke A
+ Author Affiliations
- Author Affiliations

A Faculty of Land and Food Systems, University of British Columbia, Vancouver, BC V6T 1Z4, Canada.

B Faculty of Forestry, University of British Columbia, Vancouver, BC, V6T 1Z4, Canada.

C Corresponding author. Email: maja.krzic@ubc.ca

Soil Research 58(4) 364-370 https://doi.org/10.1071/SR19180
Submitted: 5 July 2019  Accepted: 3 February 2020   Published: 31 March 2020

Abstract

Grassland set-asides (GLSA) are fields that are taken out of intensive annual crop production and seeded with a mixture of grasses and legumes for one to four years to improve soil quality. The objectives of this study were to evaluate (i) the relationships among soil organic carbon (SOC), permanganate oxidisable C (POXC), dilute-acid extractable polysaccharides (DAEP) and aggregate stability to determine if they may be used as proxies for one another, (ii) whether these indicators could be used to predict aggregate stability, (iii) if differences in soil quality after short-term GLSAs, detected with aggregate stability, could instead be detected with POXC or DAEP and (iv) potential use of diffuse Fourier transform spectroscopy (FT-MIR) to predict POXC, DAEP and aggregate stability in the Fraser River Delta region of British Columbia, Canada. There were strong relationships among SOC, POXC and DAEP, but the relationship between DAEP and SOC (R2 = 0.60, P < 0.0001) was less strong than that observed between POXC and SOC (R2 = 0.71, P < 0.0001). All three soil C fractions were significantly predicted with the 2–6 mm aggregate size fraction but the correlations for DAEP (R2 = 0.43) and POXC (R2 = 0.36) were stronger than that for SOC (R2 = 0.29). Predictions of soil quality indicators using FT-MIR produced R2 = 0.92 for POXC, R2 = 0.93 for DAEP and R2 = 0.62 for the 2–6 mm aggregate size fraction. These results suggest that FT-MIR holds promise as a low-cost method to determine labile soil C fractions that are better proxy soil quality indicators for aggregate stability than SOC.

Additional keywords: agriculture, labile carbon fractions, permanganate oxidisable carbon, perennial grass systems, soil polysaccharides, soil structure.


References

Bellon-Maurel V, McBratney A (2011) Near-infrared (NIR) and mid-infrared (MIR) spectroscopic techniques for assessing the amount of carbon stock in soils: critical review and research perspectives. Soil Biology and Biochemistry 43, 1398–1410.
Near-infrared (NIR) and mid-infrared (MIR) spectroscopic techniques for assessing the amount of carbon stock in soils: critical review and research perspectives.Crossref | GoogleScholarGoogle Scholar |

Calderón F, Culman S, Johan S, Franzluebbers AJ, Schipanski M, Beniston J, Grandy S, Kong A (2017) Quantification of soil permanganate oxidizable C (POXC) using infrared spectroscopy. Soil Science Society of America Journal 81, 277–288.
Quantification of soil permanganate oxidizable C (POXC) using infrared spectroscopy.Crossref | GoogleScholarGoogle Scholar |

Carter MR (2002) Soil quality for sustainable land management: organic matter and aggregation interactions that maintain soil functions. Agronomy Journal 94, 38–47.
Soil quality for sustainable land management: organic matter and aggregation interactions that maintain soil functions.Crossref | GoogleScholarGoogle Scholar |

Chenu C, Cosentino D (2011) Microbial regulations of soil structure dynamics. In ‘The architecture and biology of soils: life in inner space’. (Eds K Ritz, I Young) pp 37–70. (CABI: Wallingford, UK)

Culman SW, Snapp SS, Freeman MA, Schipanski ME, Beniston J, Lal R, Drinkwater LE, Franzluebbers AJ, Glover JD, Grandy AS, Lee J, Six J, Maul JE, Mirksy SB, Spargo JT, Wander MM (2012) Permanganate oxidizable carbon reflects a processed soil fraction that is sensitive to management. Soil Science Society of America Journal 76, 494–504.
Permanganate oxidizable carbon reflects a processed soil fraction that is sensitive to management.Crossref | GoogleScholarGoogle Scholar |

Delta Farmland & Wildlife Trust (2000) Farmland and wildlife: grassland set-asides (Fact Sheet #2). Delta, BC. Available at http://www.deltafarmland.ca/subpage/our-programs/grassland-set-aside-stewardship-program/ [verified 18 February 2020].

Environment Canada (2019) National climate data and information archive. Ontario. Available from http://www.climate.weatheroffice.gc.ca [verified 18 February 2020].

Fraser EDG (2004) Land tenure and agricultural management: Soil conservation on rented and owned fields in southwest British Columbia. Agriculture and Human Values 21, 73–79.
Land tenure and agricultural management: Soil conservation on rented and owned fields in southwest British Columbia.Crossref | GoogleScholarGoogle Scholar |

Gregorich EG, Carter MR, Angers DA, Monreal CM, Ellert BH (1994) Towards a minimum data set to assess soil organic matter quality in agricultural soils. Canadian Journal of Soil Science 74, 367–385.
Towards a minimum data set to assess soil organic matter quality in agricultural soils.Crossref | GoogleScholarGoogle Scholar |

Haynes RJ (2005) Labile organic matter fractions as central components of the quality of agricultural soils: an overview. Advances in Agronomy 85, 221–268.
Labile organic matter fractions as central components of the quality of agricultural soils: an overview.Crossref | GoogleScholarGoogle Scholar |

Hermawan B, Bomke AA (1996) Aggregation of a degraded lowland soil during restoration with different cropping and drainage regimes. Soil Technology 9, 239–250.
Aggregation of a degraded lowland soil during restoration with different cropping and drainage regimes.Crossref | GoogleScholarGoogle Scholar |

Hurisso TT, Culman SW, Horwath WR, Wade J, Cass D, Beniston JW, Bowles TM, Grandy AS, Franzluebbers AJ, Schipanski ME, Lucas ST, Ugarte CM (2016) Comparison of permanganate-oxidizable carbon and mineralizable carbon for assessment of organic matter stabilization and mineralization. Soil Science Society of America Journal 80, 1352–1364.
Comparison of permanganate-oxidizable carbon and mineralizable carbon for assessment of organic matter stabilization and mineralization.Crossref | GoogleScholarGoogle Scholar |

Idowu OJ, Kircher P (2016) Soil quality of semi-arid conservation reserve program lands in Eastern New Mexico. Arid Land Research and Management 30, 153–165.
Soil quality of semi-arid conservation reserve program lands in Eastern New Mexico.Crossref | GoogleScholarGoogle Scholar |

IUSS Working Group WRB (2007) ‘World Reference Base for Soil Resources 2006, first update 2007.’ World Soil Resources Reports No. 103. (FAO: Rome)

Karlen DL, Rosek MJ, Gardner JC, Allan DL (1999) Conservation Reserve Program effects on soil quality indicators. Journal of Soil and Water Conservation 54, 439–444.

Kennedy AC, Papendick RI (1995) Microbial characteristics of soil quality. Journal of Soil and Water Conservation 50, 243–248.

Lewis DB, Kaye JP, Jabbour R, Barbercheck ME (2011) Labile carbon and other soil quality indicators in two tillage systems during transition to organic agriculture. Renewable Agriculture and Food Systems 26, 342–353.
Labile carbon and other soil quality indicators in two tillage systems during transition to organic agriculture.Crossref | GoogleScholarGoogle Scholar |

Liu A, Ma BL, Bomke AA (2005) Effects of cover crops on soil aggregate stability, total organic carbon, and polysaccharides. Soil Science Society of America Journal 69, 2041–2048.
Effects of cover crops on soil aggregate stability, total organic carbon, and polysaccharides.Crossref | GoogleScholarGoogle Scholar |

Lowe LE (1993) Total and labile polysaccharide analysis of soils. In: ‘Soil sampling methods and analysis’. (Ed. MR Carter) pp. 373–376. (Canadian Soil Science Society, Lewis Publishers, Boca Raton, FL, USA)

Lussier JM, Krzic M, Smukler SM, Bomke AA, Bondar D (2019) Short-term effects of grassland set-asides on soil properties in the Fraser River Delta of British Columbia. Canadian Journal of Soil Science 99, 136–145.
Short-term effects of grassland set-asides on soil properties in the Fraser River Delta of British Columbia.Crossref | GoogleScholarGoogle Scholar |

Luttmerding HA (1981) Soils of the Langley-Vancouver map area, RAB Bull. 18, vol. 3, BC Min. Environ., Kelowna, BC.

Movasaghi Z, Rehman S, Rehman I (2008) Fourier transform infrared (FTIR) spectroscopy of biological tissues. Applied Spectroscopy Reviews 43, 134–179.
Fourier transform infrared (FTIR) spectroscopy of biological tissues.Crossref | GoogleScholarGoogle Scholar |

Nimmo JR, Perkins KS (2002) Aggregate stability and size distribution. In: ‘Methods of soil analysis, Part 4: Physical methods’. (Eds JH Dane, GC Topp Eds) pp. 317–328. (Soil Science Society of America: Madison, WI, USA)

R Core Team (2017) R: A language and environment for statistical computing. R Foundation for Statistical Computing, Vienna, Austria. Available from http://www.R-project.org/ [verified 18 February 2020].

Reeves JB, McCarthy GW, Reeves VB (2001) Mid-infrared diffuse reflectance spectroscopy for the quantitative analysis of agricultural soils. Journal of Agricultural and Food Chemistry 49, 766–772.
Mid-infrared diffuse reflectance spectroscopy for the quantitative analysis of agricultural soils.Crossref | GoogleScholarGoogle Scholar | 11262026PubMed |

Soriano-Disla JM, Janik LJ, Viscarra Rossel RA, Macdonald LM, Mclaughlin MJ (2014) The performance of visible, near-, and mid-infrared reflectance spectroscopy for prediction of soil physical, chemical, and biological properties. Applied Spectroscopy Reviews 49, 139–186.
The performance of visible, near-, and mid-infrared reflectance spectroscopy for prediction of soil physical, chemical, and biological properties.Crossref | GoogleScholarGoogle Scholar |

Thiel B, Smukler SM, Krzic M, Gergel S, Terpsma C (2015) Using hedgerow biodiversity to enhance the carbon storage of farmland in the Fraser River delta of British Columbia. Journal of Soil and Water Conservation 70, 247–256.
Using hedgerow biodiversity to enhance the carbon storage of farmland in the Fraser River delta of British Columbia.Crossref | GoogleScholarGoogle Scholar |

Veum KS, Goyne KW, Kremer RJ, Miles RJ, Sudduth KA (2014) Biological indicators of soil quality and soil organic matter characteristics in an agricultural management continuum. Biogeochemistry 117, 81–99.
Biological indicators of soil quality and soil organic matter characteristics in an agricultural management continuum.Crossref | GoogleScholarGoogle Scholar |

Walji K 2017. Nitrogen dynamics following incorporation of 3-year old grassland set-asides in Delta, British Columbia. MSc Thesis, University of British Columbia, Vancouver, Canada.

Wallace BM, Krzic M, Forge TA, Broersma K, Newman RF (2009) Biosolids increase soil aggregation and protection of soil carbon five years after application on a crested wheatgrass pasture. Journal of Environmental Quality 38, 291–298.
Biosolids increase soil aggregation and protection of soil carbon five years after application on a crested wheatgrass pasture.Crossref | GoogleScholarGoogle Scholar | 19141819PubMed |

Weil RR, Islam KR, Stine MA, Gruver JB, Samson-Liebig SE (2003) Estimating active carbon for soil quality assessment: A simplified method for laboratory and field use. American Journal of Alternative Agriculture 18, 3–17.
Estimating active carbon for soil quality assessment: A simplified method for laboratory and field use.Crossref | GoogleScholarGoogle Scholar |

Yates DE, Krzic M, Smukler SM, Bradfield G, Bomke AA, Terpsma C (2017) Comparison of selected soil properties following grassland set-aside and annual crop rotation in the Fraser River delta of British Columbia. Canadian Journal of Soil Science 97, 783–788.
Comparison of selected soil properties following grassland set-aside and annual crop rotation in the Fraser River delta of British Columbia.Crossref | GoogleScholarGoogle Scholar |