David C Coleman
Biographic Data
| ID | 9092652 |
|---|---|
| NAME | David C Coleman |
| GIVEN NAMES | David C |
| FAMILY NAME | Coleman |
| SIGNATURE | COLEMAN D C |
| AFFILIATIONS | Colorado State University |
| ORCID | 0000-0003-0390-1501 |
| VERIFIED | Yes |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 4 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1979 |
| LATEST PUBLICATION YEAR | 2017 |
| H-INDEX | 0 |
Soil Biology and Organisms
Soils are a haven for many phyla of countless numbers of microbes and fauna. The trophic (feeding) interactions between them provide much of the ecological stability of soil systems. Within the web of soil fauna, interactions occur via numerous biogeochemical cycles of the major nutrients, including carbon, nitrogen, phosphorus, and sulfur. These cycles are in turn influenced by aboveground and belowground interactions of plants and biota. Recent…
Creating Christian Granada
Creating Christian Granada provides a richly detailed examination of a critical and transitional episode in Spain's march to global empire. The city of Granada—Islam's final bastion on the Iberian peninsula—surrendered to the control of Spain's "Catholic Monarchs" Isabella and Ferdinand on January 2, 1492. Over the following century, Spanish state and Church officials, along with tens of thousands of Christian immigrant settlers, transformed the …
Amoebal growth in soil microcosms
Associations of terrestrial bacteria and amoebae provide a model system for understanding element dynamics mediated by trophic relationships in soil ecosystems. A Pseudomonas sp. and Acanthamoeba sp. were chosen for inoculation into soil sterilized with propylene oxide after screening bacterial and amoebal isolates from blue grama [Bouteloua gracilis (H.B.K.) Lag.] rhizospheres for compatibility and activity. Carbon, nitrogen, and phosphorus upta…
The use of soil microcosms in evaluating bacteriophagic nematode responses to other organisms and effects on nutrient cycling
Soil microcosms were found useful in evaluating bacteriophagic nematode population responses to biotic interactions. Bacterial and amoebal numbers were significantly decreased in the presence of an omnivorous nematode with a corresponding increase in the nematode numbers. Nematode numbers were lower in finer textured soils compared to coarser soils. Under some developmental stages, nematodes were found to increase the mineralization rate of nitro…
No prominent works on this page.
Amoebal growth in soil microcosms
Associations of terrestrial bacteria and amoebae provide a model system for understanding element dynamics mediated by trophic relationships in soil ecosystems. A Pseudomonas sp. and Acanthamoeba sp. were chosen for inoculation into soil sterilized with propylene oxide after screening bacterial and amoebal isolates from blue grama [Bouteloua gracilis (H.B.K.) Lag.] rhizospheres for compatibility and activity. Carbon, nitrogen, and phosphorus upta…
The use of soil microcosms in evaluating bacteriophagic nematode responses to other organisms and effects on nutrient cycling
Soil microcosms were found useful in evaluating bacteriophagic nematode population responses to biotic interactions. Bacterial and amoebal numbers were significantly decreased in the presence of an omnivorous nematode with a corresponding increase in the nematode numbers. Nematode numbers were lower in finer textured soils compared to coarser soils. Under some developmental stages, nematodes were found to increase the mineralization rate of nitro…
Creating Christian Granada
Creating Christian Granada provides a richly detailed examination of a critical and transitional episode in Spain's march to global empire. The city of Granada—Islam's final bastion on the Iberian peninsula—surrendered to the control of Spain's "Catholic Monarchs" Isabella and Ferdinand on January 2, 1492. Over the following century, Spanish state and Church officials, along with tens of thousands of Christian immigrant settlers, transformed the …
Soil Biology and Organisms
Soils are a haven for many phyla of countless numbers of microbes and fauna. The trophic (feeding) interactions between them provide much of the ecological stability of soil systems. Within the web of soil fauna, interactions occur via numerous biogeochemical cycles of the major nutrients, including carbon, nitrogen, phosphorus, and sulfur. These cycles are in turn influenced by aboveground and belowground interactions of plants and biota. Recent…
Biology (3 works) · Ecology (3 works) · Chemistry (2 works) · Ecology (2 works) · Ecosystem (2 works) · Microcosm (2 works) · Nutrient (2 works) · Soil water (2 works) · Trophic level (2 works) · Agronomy (1 work)