Jon Botthoff
Biographic Data
| ID | 7992348 |
|---|---|
| NAME | Jon Botthoff |
| GIVEN NAMES | Jon |
| FAMILY NAME | Botthoff |
| SIGNATURE | BOTTHOFF J |
| AFFILIATIONS | University of California, Riverside |
| VERIFIED | No |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 2 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2020 |
| LATEST PUBLICATION YEAR | 2023 |
| H-INDEX | 0 |
Soil NH3 emissions across an aridity, soil pH, and N deposition gradient in southern California
Soil ammonia (NH3) emissions are seldom included in ecosystem nutrient budgets; however, they may represent substantial pathways for ecosystem nitrogen (N) loss, especially in arid regions where hydrologic N losses are comparatively small. To characterize how multiple factors affect soil NH3 emissions, we measured NH3 losses from 6 dryland sites along a gradient in soil pH, atmospheric N deposition, and rainfall. We also enriched soils with ammon…
Continental-scale patterns of extracellular enzyme activity in the subsoil
Chemical stabilization of microbial-derived products such as extracellular enzymes (EE) onto mineral surfaces has gained attention as a possibly important mechanism leading to the persistence of soil organic carbon (SOC). While the controls on EE activities and their stabilization in the surface soil are reasonably well-understood, how these activities change with soil depth and possibly diverge from those at the soil surface due to distinct phys…
No prominent works on this page.
Continental-scale patterns of extracellular enzyme activity in the subsoil
Chemical stabilization of microbial-derived products such as extracellular enzymes (EE) onto mineral surfaces has gained attention as a possibly important mechanism leading to the persistence of soil organic carbon (SOC). While the controls on EE activities and their stabilization in the surface soil are reasonably well-understood, how these activities change with soil depth and possibly diverge from those at the soil surface due to distinct phys…
Soil NH3 emissions across an aridity, soil pH, and N deposition gradient in southern California
Soil ammonia (NH3) emissions are seldom included in ecosystem nutrient budgets; however, they may represent substantial pathways for ecosystem nitrogen (N) loss, especially in arid regions where hydrologic N losses are comparatively small. To characterize how multiple factors affect soil NH3 emissions, we measured NH3 losses from 6 dryland sites along a gradient in soil pH, atmospheric N deposition, and rainfall. We also enriched soils with ammon…
Biology (2 works) · Chemistry (2 works) · Ecology (2 works) · Environmental Chemistry (2 works) · Environmental Science (2 works) · Soil and Water Nutrient Dynamics (2 works) · Soil Carbon and Nitrogen Dynamics (2 works) · Soil Science (2 works) · Soil water (2 works) · Agronomy (1 work)