Article
Soil Science
Jiyu Jia, Jiangzhou Zhang, Yizan Li, Liz Koziol, Laura Podzikowski, Manuel Delgado-Baquerizo, Guangzhou Wang, Junling Zhang
Summary: Soil salinization is a global problem impacting food production, and increasing soil organic matter (SOM) can alleviate salt stress. The effects of soil salinity and SOM on microbial diversity and activities were examined. Bacterial diversity, but not fungal diversity, showed significant positive relationships with soil multifunctionality (SMF) under high SOM (>15 mg/kg) and low EC (<4 ds/m) conditions. Sensitive bacteria were more strongly correlated with SMF than non-sensitive bacteria. SOM directly and indirectly impacted SMF through changes in sensitive bacterial abundance, while soil EC impacted SMF via altered sensitive bacterial diversity. Carbon and micronutrient cycling were mainly determined by bacterial diversity. Coupling decreased salinization with increased SOM can enhance soil multifunctionality by increasing the diversity and abundance of sensitive soil microbes.
Article
Soil Science
Ya Wang, Simin Wang, Chengzhu Liu, Erxiong Zhu, Juan Jia, Xiaojuan Feng
Summary: The relationship between soil organic matter (SOM) diversity and soil organic carbon (SOC) persistence is understudied in high-SOC soils such as wetlands. This study investigated shifts in SOM diversity after drainage in three wetland sites of varying SOC concentrations. The results showed that SOM diversity had a non-linear relationship with SOC concentration, with low-SOC wetlands exhibiting an increase in SOM diversity after drainage, while high-SOC wetlands did not show any change. Factors such as plant inputs and microbial processing influenced SOM diversity in high-SOC wetlands. These findings provide new insights into wetland SOC stability in the context of drainage.
Article
Soil Science
Matthias Waibel, Kevin McDonnell, Maria Tuohy, Sally Shirran, Sylvia Synowsky, Barry Thornton, Eric Paterson, Fiona Brennan, Florence Abram
Summary: Soil organic matter (SOM) is complex and important for providing nutrients to plants. Understanding SOM utilisation processes can improve fertiliser management for plant growth and reduce environmental losses. Metaproteomics can characterise protein profiles and provide insights into SOM microbial decomposition mechanisms. This study applied different extraction methods to recover SOM with different characteristics in two soil types and analysed peptide identification using liquid chromatography and tandem mass spectrometry. The results showed contrasting protein and humic substance content in different extracts, and diverse peptide hits associated with Proteobacteria and derived taxa. This work suggests areas for optimisation in chromatography and mass spectrometry to characterise SOM-associated metaproteomes.
EUROPEAN JOURNAL OF SOIL SCIENCE
(2023)
Article
Engineering, Environmental
Hang Li, Garrett McKay
Summary: The reducibility of DOM by sodium borohydride varied significantly among different DOM samples, with soil humic substances being less reducible than aquatic humic substances. While there were statistically significant correlations between the reducibility of DOM and molecular size descriptors, these descriptors could not differentiate between soil and aquatic DOM isolates with similar bulk properties. The extent of absorbance removal by borohydride is largely determined by the origin of the humic substance isolate (aquatic vs soil) instead of molecular size or charge.
ENVIRONMENTAL SCIENCE & TECHNOLOGY
(2021)
Article
Soil Science
YunFei Zhao, Xia Wang, Fei Chen, Jia Li, JinHong Wu, YuXin Sun, YuanYe Zhang, Tao Deng, SiLong Jiang, XiaoHe Zhou, HuiYing Liu
Summary: In this study, the link between aboveground biomass (AGB) and soil organic matter (SOM) across 209 alpine grassland sites on the Tibetan Plateau was evaluated. It was found that AGB decreased with increasing aridity severity above a threshold of 0.37. Additionally, a stronger positive relationship between AGB and SOM was observed in more arid conditions beyond an aridity threshold of 0.64. The results highlight the importance of soil carbon sequestration strategies for biomass production and climate change mitigation in arid areas.
Article
Soil Science
Karen Baumann, Kai-Uwe Eckhardt, Ingo Schoening, Marion Schrumpf, Peter Leinweber
Summary: The study found that grassland management plays a significant role in influencing the composition and stability of soil organic matter (SOM), impacting the dynamics of SOM in grasslands. However, the proportion and composition of the soil clay fraction, particularly when the soil clay/OC ratio is low, can override the effects of grassland management on SOM composition and stability.
SOIL USE AND MANAGEMENT
(2022)
Article
Environmental Sciences
Youhei Yamashita, Daiki Kojima, Natsumi Yoshida, Hideaki Shibata
Summary: Atmospheric deposition of soot is likely a major source of dissolved black carbon (DBC) in streams, which is linearly related to dissolved organic carbon (DOC) concentration. The quality of DBC correlates with qualitative parameters of bulk dissolved organic matter (DOM), indicating a linkage between the transfer mechanism of soot-derived DBC and high-molecular-weight aromatic DOM.
Article
Environmental Sciences
Fernanda Santos, Elizabeth Herndon
Summary: Manganese (Mn) is a crucial micronutrient for plants, as it plays a critical role in oxidizing and degrading complex organic molecules during litter decomposition. Previous studies have shown a negative correlation between Mn concentrations and carbon (C) storage in organic horizons, suggesting that high Mn concentrations in leaf litter reduce soil C storage in forest ecosystems. However, the relationship between Mn and C in the litter layer and organic soil remains poorly understood. To investigate this relationship across different ecosystems, we analyzed biogeochemical data from the National Ecological Observatory Network (NEON) database. Our findings show that increased C and nitrogen (N) storage in organic horizons are associated with decreased Mn concentrations in diverse ecosystems. This correlation is linked to the degree of organic matter decomposition and is stronger than the correlation with climatic variables. Additionally, foliar Mn and lignin content are strongly correlated, and both increase with decreasing soil pH, suggesting a connection between soil pH, foliar chemistry, and litter decomposability. Our observations indicate that higher Mn bioavailability and accumulation in foliage under moderately acidic soil conditions promote fungal decomposition of lignin-rich litter and contribute to lower soil C stocks.
GLOBAL BIOGEOCHEMICAL CYCLES
(2023)
Article
Environmental Sciences
Marina Feraud, Patricia A. Holden
Summary: This study investigated the content and sources of metal elements in suburban bioswales and proposed a transferable soil management decision-making method to ensure that soil metal concentrations meet ecological screening standards.
SCIENCE OF THE TOTAL ENVIRONMENT
(2021)
Article
Soil Science
Aaron L. Frankl, Daniel P. Maxbauer, Mary E. Savina
Summary: The study revealed a relationship between soil magnetic properties and soil organic matter (SOM) in agricultural fields, with strong positive correlations between SOM and specific magnetic properties. The presence of fine-grained magnetite/maghemite in well-drained soils during pedogenesis contributes to the sensitivity of magnetic properties to SOM. Despite differences in management strategies, the correlation persists, supporting the functional link between SOM and soil-formed magnetic minerals.
Article
Environmental Sciences
Katherine S. Rocci, Jocelyn M. Lavallee, Catherine E. Stewart, M. Francesca Cotrufo
Summary: Soil organic carbon (SOC) dynamics are influenced by global changes like nitrogen fertilization, elevated CO2, warming, and increased precipitation. Particulate organic carbon (POC) is more responsive in the short-term, while nitrogen fertilization has a dominant impact on increasing SOC. Long-term experiments and individual studies on different forms of organic carbon responses to global changes are crucial for a better understanding of SOC dynamics.
SCIENCE OF THE TOTAL ENVIRONMENT
(2021)
Article
Agriculture, Multidisciplinary
A. G. El-Naggar, C. B. Hedley, P. Roudier, D. Horne, B. E. Clothier
Summary: This study developed a quasi-2-dimensional inversion model based on electromagnetic induction surveys to derive true electrical conductivity and volumetric water content of the soil profile, establishing relationships between the two properties. The method was applied for irrigation scheduling and monitoring spatio-temporal variations of soil moisture, showing potential for predicting 2D depth profiles of soil characteristics and supporting soil management.
PRECISION AGRICULTURE
(2021)
Article
Ecology
Gregory S. Richardson, Matthew D. Ruark, Timothy Radatz, Amber Radatz, Eric Cooley, Erin M. Silva, Abigail J. Augarten, Jun Zhu, Chelsea H. Zegler
Summary: The accumulation of soil organic matter (SOM) is crucial for the functioning of agroecosystems. However, the influence of soil properties and agricultural management practices on SOM dynamics is often overlooked. This study used a network of farm fields in the USA to assess the effects of soil properties and management variables on SOM, total organic carbon (TOC), and total nitrogen (TN). The results showed that poorly drained soil, tile-drained fields, high clay content soil, and high biomass crop rotations were associated with greater SOM, TOC, and TN.
Article
Agronomy
Marcin Becher, Miroslaw Kobierski, Krzysztof Pakula, Dawid Jaremko
Summary: The secondary transformation of organic matter in drained peatlands of the temperate climate zone has a significant effect on the total mercury content and stock in soils. This research is of great importance for soil monitoring and planning the restoration of peatlands.
Article
Environmental Sciences
Edward Tipping, Jessica L. Elias, Patrick O. Keenan, Rachel C. Helliwell, Nikolai Pedentchouk, Richard J. Cooper, Sarah Buckingham, Egil Gjessing, Philippa Ascough, Charlotte L. Bryant, Mark H. Garnett
Summary: This study investigated the concentrations and properties of dissolved organic carbon (DOC) in rivers in relation to terrestrial source solutions at a global scale. The study found significant differences in DOC concentrations and properties among different terrestrial sources, which were explained by optimizing the simulated riverine variables and combinations of source waters. In rivers draining forests and grass-shrub land cover, most of the DOC comes from topsoil and subsoil, with a small contribution from groundwater. In cropland rivers, subsoil and groundwater are the dominant sources of DOC, while in wetland rivers, most of the DOC is from topsoil.
SCIENCE OF THE TOTAL ENVIRONMENT
(2022)