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Deep-rooted perennials alter microbial respiration and chemical composition of carbon in density fractions along soil depth profiles

Journal Article · · Geoderma
 [1];  [2];  [3];  [2];  [2];  [2];  [4];  [5];  [6];  [7];  [4]
  1. Seoul National Univ. (Korea, Republic of); Univ. of California, Merced, CA (United States)
  2. Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)
  3. Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States); Yale Univ., New Haven, CT (United States)
  4. Univ. of California, Merced, CA (United States)
  5. Univ. of Wisconsin, Madison, WI (United States)
  6. Michigan State Univ., East Lansing, MI (United States)
  7. Univ. of California, Merced, CA (United States); Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)
Growing deep-rooted perennials has been proposed to increase soil organic carbon (SOC) stocks and mitigate CO2 emissions. Yet, we know little about the bioavailability and chemical properties of SOC under deep-rooted perennials and shallow-rooted annuals. Improving our understanding of the role of deep-rooted perennials for belowground C storage is critical, as root growth has the potential to both increase SOC stock and accelerate loss of existing SOC. Here, we assessed the effects of >10 years of land conversion from shallow-rooted annuals (maize) to deep-rooted perennials (switchgrass) on SOC bioavailability (microbial respiration, Δ14C-CO2), mineral-associated SOC (density fractionation), and SOC turnover and composition (14C-SOC, DRIFT spectroscopy) in surface soils (0–20 cm) and subsoils (90–120 cm) at two sites with sandy and silty soils. We demonstrate that switchgrass enhanced microbial respiration of recently-fixed C in surface soils. Switchgrass increased Δ14C values of the free light fraction in subsoil of the sandy site, by supplying aliphatic C (putative simple plant C) into the soil. In contrast, maize input less root C into the soil, and at one site increased the decomposition of older SOC, which indicates that overall microbial C demand outpaced plant C inputs. These results highlight that deep-rooted perennials stimulate the transfer of more atmospheric C to both surface and subsoils than shallow-rooted annuals, that newly generated SOC under deep-rooted perennials is relatively less protected from decomposition, and that reaping the C benefits of deep-rooted perennials could require maintaining the land cover as a perennial cropping system.
Research Organization:
Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)
Sponsoring Organization:
Korea Environmental Industry & Technology Institute (KEITI); National Research Foundation of Korea (NRF); National Science Foundation (NSF); USDA; USDOE; USDOE Laboratory Directed Research and Development (LDRD) Program; USDOE National Nuclear Security Administration (NNSA); USDOE Office of Science (SC), Biological and Environmental Research (BER)
Grant/Contract Number:
AC52-07NA27344; SC0018409
OSTI ID:
2520214
Alternate ID(s):
OSTI ID: 2575668
OSTI ID: 2530267
Report Number(s):
LLNL--JRNL-868298; LLNL--JRNL-870245; 1104304
Journal Information:
Geoderma, Journal Name: Geoderma Vol. 455; ISSN 0016-7061
Publisher:
ElsevierCopyright Statement
Country of Publication:
United States
Language:
English

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