Effect of coagulation on a model planktonic food web
By G. Jackson. 2001
103 citations recorded by the source corpus.
Subfields: Ecology, Oceanography
View Paper: https://www.semanticscholar.org/paper/916db588247f28431a40802ffb537828421f7475
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Ecology
- Hans-Peter Grossart
- H. Ploug
- M. Simon
- B. Schweitzer
- Michael J. Behrenfeld
- T. Kiørboe
- Emmanuel S. Boss
- A. Milligan
In Oceanography
- H. Ploug
- T. Kiørboe
- Hans-Peter Grossart
- Michael J. Behrenfeld
- M. Simon
- B. Schweitzer
- Emmanuel S. Boss
- L. Karp‐Boss
Citations in the corpus
- Pelagic functional group modeling: Progress, challenges and prospects (2006, unknown): “…sophisticated mechanistic formulations that take into account factors such as particle ‘‘stickiness’’ and collision rate in coagulation processes (e.g., Jackson, 1990, 2001) to simple parameterizations in biogeochemical models that accelerate sinking rate when phytoplankton concentrations are high…”
- Thoughts on the evolution and ecological niche of diatoms (2021, background): “One simple explanation for such events is that high abundance leads to more cells “bumping into each other” (i.e., higher encounter), creating sinking aggregates (Kiorboe 1993, Jackson 2001).”
- Microbial ecology of organic aggregates in aquatic ecosystems (2002, background): “…heterogeneities of nutrients in the bulk water, which may affect nutrient recycling and colonization processes by chemotactic microorganisms and remote chemosensoric detection by meso- and macrozooplankton (Kiørboe 2001, Kiørboe & Jackson 2001, Kiørboe & Thygesen 2001, Kiørboe et al. 2001).”
- Formation and fate of marine snow: small-scale processes with large- scale implications (2001, methodology): “…may constitute a quantitatively important source of DOM for free-living bacteria and the solute plume surrounding the sinking aggregate an important growth habitat for bacteria (Kiør- ˆ ˆ * B m a F a B pm p S = = −β µ db dt B B pBF dF dt aBF mF S= + − = − β µ 68 T. KIØRBOE boe and Jackson, 2001).”