1990
DOI: 10.1007/bf00002062
|View full text |Cite
|
Sign up to set email alerts
|

Carbon and nitrogen cycling during old-field succession: Constraints on plant and microbial biomass

Abstract: Soil C and N dynamics were studied in a sequence of old fields of increasing age to determine how these biogeochemical cycles change during secondary succession. In addition, three different late-successional forests were studied to represent possible "steady state" conditions. Surface soil samples collected from the fields and forests were analyzed for total C, H,O-soluble C, total N, potential net N mineralization, potential net nitrification, and microbial biomass. Aboveand belowground plant biomass was est… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1

Citation Types

9
129
2
4

Year Published

2000
2000
2024
2024

Publication Types

Select...
9
1

Relationship

2
8

Authors

Journals

citations
Cited by 180 publications
(144 citation statements)
references
References 36 publications
9
129
2
4
Order By: Relevance
“…The 16 species treatment is thus representative of high-diversity native vegetation, whereas one, two, and four species treatments have diversity similar to potential biomass crops (i.e., grasses grown as monocultures) and to other regional grasslands of anthropogenic origin (but might have lower productivity than biomass crops chosen because they have high productivity). Because soil N mineralization rates at our site (22) range from ∼34 to 80 kg N·ha −1 ·y −1 , addition of as much as ∼50 kg N·ha −1 ·y −1 would move a system from low to high soil N status. The five driest years of the past 150 y had growing season precipitation approximately 50% less than the mean, and the five wettest approximately 50% greater than the mean (23), placing our water treatments within this range of observed climatic variation.…”
Section: Resultsmentioning
confidence: 99%
“…The 16 species treatment is thus representative of high-diversity native vegetation, whereas one, two, and four species treatments have diversity similar to potential biomass crops (i.e., grasses grown as monocultures) and to other regional grasslands of anthropogenic origin (but might have lower productivity than biomass crops chosen because they have high productivity). Because soil N mineralization rates at our site (22) range from ∼34 to 80 kg N·ha −1 ·y −1 , addition of as much as ∼50 kg N·ha −1 ·y −1 would move a system from low to high soil N status. The five driest years of the past 150 y had growing season precipitation approximately 50% less than the mean, and the five wettest approximately 50% greater than the mean (23), placing our water treatments within this range of observed climatic variation.…”
Section: Resultsmentioning
confidence: 99%
“…The positive relationship of the 16S rRNA gene to % C can be attributed to microbial heterotrophic metabolism (Zak et al, 1990). A similar relationship between nifH, nirS, nirK, and nosZ and % C can also be explained given the heterotrophic nature of the organisms which carry these genes (Knowles, 1982).…”
Section: Discussionmentioning
confidence: 98%
“…The time taken for the equilibrium state to develop was estimated to be 10 years following natural forest succession in Nigeria (0-10 cm, Aweto 1981), 30 years under eucalyptus and pine plantations in Congo (0-5 cm, Trouve et al 1996), 40-60 years under pine-oak stands in Massachusetts (0-15 cm, Compton et al 1998), and more than 60 years following natural forest succession in Minnesota (0-10 cm, Zak et al 1990). In our study, shrubs and trees had grown for 25 years since plantation.…”
Section: Discussionmentioning
confidence: 99%