2000
DOI: 10.1007/s003749900189
|View full text |Cite
|
Sign up to set email alerts
|

Soil-released carbon dioxide from microbial biomass carbon in the cultivated soils of karst areas of southwest China

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1

Citation Types

1
5
0

Year Published

2001
2001
2024
2024

Publication Types

Select...
8
1

Relationship

0
9

Authors

Journals

citations
Cited by 27 publications
(6 citation statements)
references
References 19 publications
1
5
0
Order By: Relevance
“…The 1-box model enabled us to estimate the time until 95% of the C in a pool was replaced, which corresponds to 3τ. In accordance with our estimate, the mean τs of the dynamic C pools of soils from the US corn belt were 100 days (Collins et al 2000) and those of microbial biomass C from Chinese karst soils were 105 days (Piao et al 2000).…”
supporting
confidence: 89%
“…The 1-box model enabled us to estimate the time until 95% of the C in a pool was replaced, which corresponds to 3τ. In accordance with our estimate, the mean τs of the dynamic C pools of soils from the US corn belt were 100 days (Collins et al 2000) and those of microbial biomass C from Chinese karst soils were 105 days (Piao et al 2000).…”
supporting
confidence: 89%
“…The lack of this flush may be the main reason why in this study the CO 2 evolution rate amounted to only 6% of that measured in an 18-day laboratory study with a similar soil, which was sun-dried and rewetted (Wichern et al, 2003). The CO 2 evolution rates of the present study are within the range of 0-300 mg CO 2 -C m −2 h −1 obtained by others using the static chamber method for field measurements at arable sites in humid temper- Table 2 Weighted mean, minimum and maximum of the CO 2 evolution rate and of the soil temperature at 5 cm depth during the measurement of the CO 2 evolution rate over a 12-day irrigation cycle for three plot types at the oasis of Balad Seet, Oman ate regions (Franzluebbers et al, 1995;Jensen et al, 1996;Piao et al, 2000). In addition, they are also in the range of those results obtained with the dynamic chamber method in humid temperate regions (Jensen et al, 1996).…”
Section: Resultsmentioning
confidence: 99%
“…As the epicenter of karst landforms in Southwest China, Guizhou Province stands as one of the country's largest and most extensive typical karst areas (He et al 2022). Owing to soil acidi cation and erosion, there has been signi cant loss of soil nutrients and a sharp decline in productivity, with yellow and limestone soils being the predominant soil types in this region (Piao et al 2000;Zhou et al 2023). Given the ongoing destruction of the ecological environment and economic regression, animal husbandry emerges as a promising avenue to both restore the environment and promote economic development of the area (Song et al 2018).…”
Section: Introductionmentioning
confidence: 99%