2021
DOI: 10.1029/2021jg006352
|View full text |Cite
|
Sign up to set email alerts
|

Dissolved Organic Matter Dynamics in Reference and Calcium Silicate‐Treated Watersheds at Hubbard Brook Experimental Forest, NH, USA

Abstract: Dissolved organic matter (DOM) plays a critical role in the transfer of energy and nutrients within and between terrestrial and aquatic ecosystems (Jaffé et al., 2008). Soils have the capacity to store considerably more carbon than quantities found in either the atmosphere or plant biomass (Schmidt et al., 2011). A fraction of soil carbon is mobilized as DOM to drainage waters, making it one of the largest sources of organic carbon to freshwater and marine ecosystems (Battin et al., 2008).

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

2022
2022
2024
2024

Publication Types

Select...
5

Relationship

0
5

Authors

Journals

citations
Cited by 5 publications
(1 citation statement)
references
References 87 publications
(136 reference statements)
0
1
0
Order By: Relevance
“…In the short term, dissolution of lime (CaCO 3 + H 2 O → Ca 2+ + HCO 3 − + OH − ) provides hydroxide ions that directly neutralize acidity and provides calcium for cation exchange sites, raising base saturation. In the long term, ecosystem feedbacks cause indirect effects driven by the recycling of calcium in plant litter, changes in plant carbon (C) allocation to roots and microbial symbionts (Fahey et al, 2016), and the effects of Ca on organic matter quality and solubility (LoRusso et al, 2021; Rowley et al, 2018), and the CEC of organic soil horizons (Johnson et al, 2014). Direct effects of liming on microbiome composition, driven by proton concentration, should be apparent in short‐term experiments, while indirect effects are likely to manifest only after long periods of time.…”
Section: Introductionmentioning
confidence: 99%
“…In the short term, dissolution of lime (CaCO 3 + H 2 O → Ca 2+ + HCO 3 − + OH − ) provides hydroxide ions that directly neutralize acidity and provides calcium for cation exchange sites, raising base saturation. In the long term, ecosystem feedbacks cause indirect effects driven by the recycling of calcium in plant litter, changes in plant carbon (C) allocation to roots and microbial symbionts (Fahey et al, 2016), and the effects of Ca on organic matter quality and solubility (LoRusso et al, 2021; Rowley et al, 2018), and the CEC of organic soil horizons (Johnson et al, 2014). Direct effects of liming on microbiome composition, driven by proton concentration, should be apparent in short‐term experiments, while indirect effects are likely to manifest only after long periods of time.…”
Section: Introductionmentioning
confidence: 99%