89 citations as recorded by crossref.

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2. Organic matter stability and lability in terrestrial and aquatic ecosystems: A chemical and microbial perspective V. Verrone et al. 10.1016/j.scitotenv.2023.167757
3. Addressing numerical challenges in introducing a reactive transport code into a land surface model: a biogeochemical modeling proof-of-concept with CLM–PFLOTRAN 1.0 G. Tang et al. 10.5194/gmd-9-927-2016
4. Soil carbon storage controlled by interactions between geochemistry and climate S. Doetterl et al. 10.1038/ngeo2516
5. Soil organic matter accumulation in relation to changing soil volume, mass, and structure: Concepts and calculations P. Sollins & J. Gregg 10.1016/j.geoderma.2017.04.013
6. Ecological stoichiometry as a foundation for omics-enabled biogeochemical models of soil organic matter decomposition E. Graham & K. Hofmockel 10.1007/s10533-021-00851-2
7. Responses of two nonlinear microbial models to warming and increased carbon input Y. Wang et al. 10.5194/bg-13-887-2016
8. Glyphosate dispersion, degradation, and aquifer contamination in vineyards and wheat fields in the Po Valley, Italy D. la Cecilia et al. 10.1016/j.watres.2018.09.008
9. From legacy contamination to watershed systems science: a review of scientific insights and technologies developed through DOE-supported research in water and energy security D. Dwivedi et al. 10.1088/1748-9326/ac59a9
10. Hourly and daily rainfall intensification causes opposing effects on C and N emissions, storage, and leaching in dry and wet grasslands F. Tang et al. 10.1007/s10533-019-00580-7
11. Soil Organic Matter Temperature Sensitivity Cannot be Directly Inferred From Spatial Gradients R. Abramoff et al. 10.1029/2018GB006001
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13. Expanding the role of reactive transport models in critical zone processes L. Li et al. 10.1016/j.earscirev.2016.09.001
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15. Spatial Associations and Chemical Composition of Organic Carbon Sequestered in Fe, Ca, and Organic Carbon Ternary Systems T. Sowers et al. 10.1021/acs.est.8b01158
16. Effects of soil process formalisms and forcing factors on simulated organic carbon depth-distributions in soils S. Keyvanshokouhi et al. 10.1016/j.scitotenv.2018.10.236
17. Contribution of sorption, DOC transport and microbial interactions to the 14C age of a soil organic carbon profile: Insights from a calibrated process model B. Ahrens et al. 10.1016/j.soilbio.2015.06.008
18. Iron-bound organic carbon in forest soils: quantification and characterization Q. Zhao et al. 10.5194/bg-13-4777-2016
19. Improving understanding of soil organic matter dynamics by triangulating theories, measurements, and models J. Blankinship et al. 10.1007/s10533-018-0478-2
20. The effect of biologically mediated decay rates on modelling soil carbon sequestration in agricultural settings M. Davoudabadi et al. 10.1016/j.envsoft.2023.105786
21. Millennial-age glycerol dialkyl glycerol tetraethers (GDGTs) in forested mineral soils: <sup>14</sup>C-based evidence for stabilization of microbial necromass H. Gies et al. 10.5194/bg-18-189-2021
22. A sequential selective dissolution method to quantify storage and stability of organic carbon associated with Al and Fe hydroxide phases K. Heckman et al. 10.1016/j.geoderma.2017.09.043
23. Fine silt and clay content is the main factor defining maximal C and N accumulations in soils: a meta-analysis F. Matus 10.1038/s41598-021-84821-6
24. Land use change alters the radiocarbon age and composition of soil and water-soluble organic matter in the Brazilian Cerrado J. James et al. 10.1016/j.geoderma.2019.03.019
25. Combination of energy limitation and sorption capacity explains 14C depth gradients B. Ahrens et al. 10.1016/j.soilbio.2020.107912
26. Influence of hydrological, biogeochemical and temperature transients on subsurface carbon fluxes in a flood plain environment B. Arora et al. 10.1007/s10533-016-0186-8
27. Mineral properties, microbes, transport, and plant-input profiles control vertical distribution and age of soil carbon stocks D. Dwivedi et al. 10.1016/j.soilbio.2016.12.019
28. Warming‐induced global soil carbon loss attenuated by downward carbon movement Z. Luo et al. 10.1111/gcb.15370
29. Biochemical modeling of microbial memory effects and catabolite repression on soil organic carbon compounds D. la Cecilia et al. 10.1016/j.soilbio.2018.10.003
30. Zones of influence for soil organic matter dynamics: A conceptual framework for data and models C. Cagnarini et al. 10.1111/gcb.14787
31. Perennial intermediate wheatgrass accumulates more soil organic carbon than annual winter wheat – a model assessment F. Tang et al. 10.1007/s11104-023-06298-8
32. Comparison With Global Soil Radiocarbon Observations Indicates Needed Carbon Cycle Improvements in the E3SM Land Model J. Chen et al. 10.1029/2018JG004795
33. The Ability of Soil Pore Network Metrics to Predict Redox Dynamics Is Scale Dependent T. Wanzek et al. 10.3390/soilsystems2040066
34. A Theory of Effective Microbial Substrate Affinity Parameters in Variably Saturated Soils and an Example Application to Aerobic Soil Heterotrophic Respiration J. Tang & W. Riley 10.1029/2018JG004779
35. Biomodulation of Nitrogen Cycle in Suspended Sediment F. Tang & F. Maggi 10.1002/2017JG004165
36. Reactive Transport Processes that Drive Chemical Weathering: From Making Space for Water to Dismantling Continents K. Maher & A. Navarre-Sitchler 10.2138/rmg.2018.85.12
37. The Millennial model: in search of measurable pools and transformations for modeling soil carbon in the new century R. Abramoff et al. 10.1007/s10533-017-0409-7
38. Soil fungal mycelia have unexpectedly flexible stoichiometric C:N and C:P ratios T. Camenzind et al. 10.1111/ele.13632
39. Evaluation of an untargeted nano-liquid chromatography-mass spectrometry approach to expand coverage of low molecular weight dissolved organic matter in Arctic soil M. Ladd et al. 10.1038/s41598-019-42118-9
40. The Case for Digging Deeper: Soil Organic Carbon Storage, Dynamics, and Controls in Our Changing World C. Gross & R. Harrison 10.3390/soilsystems3020028
41. δ13C and 14C activity of groundwater DOC and DIC in the volcanically active and arid Loa Basin of northern Chile L. Godfrey et al. 10.1016/j.jhydrol.2021.125987
42. What are the products of enzymatic cleavage of organic N? C. Warren 10.1016/j.soilbio.2021.108152
43. Ecosystem-scale modelling of soil carbon dynamics: Time for a radical shift of perspective? P. Baveye 10.1016/j.soilbio.2023.109112
44. Differential effects of redox conditions on the decomposition of litter and soil organic matter Y. Lin et al. 10.1007/s10533-021-00790-y
45. Innovative approaches in soil carbon sequestration modelling for better prediction with limited data M. Davoudabadi et al. 10.1038/s41598-024-53516-z
46. Indexing Permafrost Soil Organic Matter Degradation Using High-Resolution Mass Spectrometry B. Mann et al. 10.1371/journal.pone.0130557
47. Biogeochemical modeling of CO<sub>2</sub> and CH<sub>4</sub> production in anoxic Arctic soil microcosms G. Tang et al. 10.5194/bg-13-5021-2016
48. SUPECA kinetics for scaling redox reactions in networks of mixed substrates and consumers and an example application to aerobic soil respiration J. Tang & W. Riley 10.5194/gmd-10-3277-2017
49. Parametrization consequences of constraining soil organic matter models by total carbon and radiocarbon using long-term field data L. Menichetti et al. 10.5194/bg-13-3003-2016
50. The changing faces of soil organic matter research P. Smith et al. 10.1111/ejss.12500
51. Dynamic Stability of Soil Carbon: Reassessing the “Permanence” of Soil Carbon Sequestration K. Dynarski et al. 10.3389/fenvs.2020.514701
52. Development of soil radiocarbon profiles in a reactive transport framework J. Druhan & C. Lawrence 10.1016/j.gca.2021.05.021
53. KEYLINK: towards a more integrative soil representation for inclusion in ecosystem scale models. I. review and model concept G. Deckmyn et al. 10.7717/peerj.9750
54. Spatiotemporal Assessment of GHG Emissions and Nutrient Sequestration Linked to Agronutrient Runoff in Global Wetlands C. Pasut et al. 10.1029/2020GB006816
55. A Mechanistic Analysis of Wetland Biogeochemistry in Response to Temperature, Vegetation, and Nutrient Input Changes C. Pasut et al. 10.1029/2019JG005437
56. Influence of land use and different plant residues on isotopic carbon distribution of total and water extractable organic matter in an incubation experiment with weathered tropical soil S. da Silva et al. 10.1002/ldr.4539
57. Assessing GHG cycling in agricultural and riparian soils using a uniform reactive transport modeling approach M. Jia et al. 10.1016/j.geoderma.2022.116078
58. Ecological and soil hydraulic implications of microbial responses to stress – A modeling analysis A. Brangarí et al. 10.1016/j.advwatres.2017.11.005
59. Abiotic and Biotic Controls on Soil Organo–Mineral Interactions: Developing Model Structures to Analyze Why Soil Organic Matter Persists D. Dwivedi et al. 10.2138/rmg.2019.85.11
60. Controls on terrestrial carbon feedbacks by productivity versus turnover in the CMIP5 Earth System Models C. Koven et al. 10.5194/bg-12-5211-2015
61. A parallelization scheme to simulate reactive transport in the subsurface environment with OGS#IPhreeqc 5.5.7-3.1.2 W. He et al. 10.5194/gmd-8-3333-2015
62. Linear two-pool models are insufficient to infer soil organic matter decomposition temperature sensitivity from incubations J. Tang & W. Riley 10.1007/s10533-020-00678-3
63. Carbon, Nitrogen, and Sulfur Elemental Fluxes in the Soil and Exchanges with the Atmosphere in Australian Tropical, Temperate, and Arid Wetlands C. Pasut et al. 10.3390/atmos12010042
64. Integrating McGill Wetland Model (MWM) with peat cohort tracking and microbial controls S. Shao et al. 10.1016/j.scitotenv.2021.151223
65. On the relationships between the Michaelis–Menten kinetics, reverse Michaelis–Menten kinetics, equilibrium chemistry approximation kinetics, and quadratic kinetics J. Tang 10.5194/gmd-8-3823-2015
66. Microbial models with minimal mineral protection can explain long-term soil organic carbon persistence D. Woolf & J. Lehmann 10.1038/s41598-019-43026-8
67. The HPx software for multicomponent reactive transport during variably-saturated flow: Recent developments and applications D. Jacques et al. 10.1515/johh-2017-0049
68. From Soils to Streams: Connecting Terrestrial Carbon Transformation, Chemical Weathering, and Solute Export Across Hydrological Regimes H. Wen et al. 10.1029/2022WR032314
69. Estimation of Permafrost SOC Stock and Turnover Time Using a Land Surface Model With Vertical Heterogeneity of Permafrost Soils S. Shu et al. 10.1029/2020GB006585
70. Weaker soil carbon–climate feedbacks resulting from microbial and abiotic interactions J. Tang & W. Riley 10.1038/nclimate2438
71. Implications of uncertain bioreactive parameters on a complex reaction network of atrazine biodegradation in soil G. Porta et al. 10.1016/j.advwatres.2018.08.002
72. Probabilistic indicators for soil and groundwater contamination risk assessment D. la Cecilia et al. 10.1016/j.ecolind.2020.106424
73. Observational needs for estimating Alaskan soil carbon stocks under current and future climate U. Vitharana et al. 10.1002/2016JG003421
74. Toward improved model structures for analyzing priming: potential pitfalls of using bulk turnover time K. Georgiou et al. 10.1111/gcb.13039
75. In-situ atrazine biodegradation dynamics in wheat ( Triticum ) crops under variable hydrologic regime D. la Cecilia & F. Maggi 10.1016/j.jconhyd.2017.05.004
76. Seasonal Biotic Processes Vary the Carbon Turnover by Up To One Order of Magnitude in Wetlands C. Pasut et al. 10.1029/2022GB007679
77. Explicitly representing soil microbial processes in Earth system models W. Wieder et al. 10.1002/2015GB005188
78. Similar importance of edaphic and climatic factors for controlling soil organic carbon stocks of the world Z. Luo et al. 10.5194/bg-18-2063-2021
79. Modeling ecosystem-scale carbon dynamics in soil: The microbial dimension J. Schimel 10.1016/j.soilbio.2023.108948
80. Synthetic iron (hydr)oxide-glucose associations in subsurface soil: Effects on decomposability of mineral associated carbon R. Porras et al. 10.1016/j.scitotenv.2017.08.290
81. A method of alternating characteristics with application to advection-dominated environmental systems K. Georgiou et al. 10.1007/s10596-018-9729-5
82. Accurate and efficient prediction of fine‐resolution hydrologic and carbon dynamic simulations from coarse‐resolution models G. Pau et al. 10.1002/2015WR017782
83. Organic vs inorganic contribution to the chemistry of cretaceous black shales in the Mamfe basin, SW Cameroon. Evidence from geochemistry and statistical analysis B. Salomon Betrant et al. 10.1016/j.heliyon.2023.e13748
84. Similarities and differences in the sensitivity of soil organic matter (SOM) dynamics to biogeochemical parameters for different vegetation inputs and climates G. Ceriotti et al. 10.1007/s00477-020-01868-z
85. Multiple models and experiments underscore large uncertainty in soil carbon dynamics B. Sulman et al. 10.1007/s10533-018-0509-z
86. The effect of temperature on the rate, affinity, and 15N fractionation of NO3 − during biological denitrification in soils F. Maggi & W. Riley 10.1007/s10533-015-0095-2
87. Are oxygen limitations under recognized regulators of organic carbon turnover in upland soils? M. Keiluweit et al. 10.1007/s10533-015-0180-6
88. Anaerobic microsites have an unaccounted role in soil carbon stabilization M. Keiluweit et al. 10.1038/s41467-017-01406-6
89. Breakdown, uptake and losses of human urine chemical compounds in barley (Hordeum vulgare) and soybean (Glycine max) agricultural plots F. Tang & F. Maggi 10.1007/s10705-016-9768-z