1986
DOI: 10.1016/s0232-4393(86)80033-6
|View full text |Cite
|
Sign up to set email alerts
|

Yeasts in soils of Egypt

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
4
1

Year Published

2004
2004
2021
2021

Publication Types

Select...
6
2

Relationship

0
8

Authors

Journals

citations
Cited by 12 publications
(5 citation statements)
references
References 9 publications
0
4
1
Order By: Relevance
“…Conversely, it is well known that the optimum growth pH range for yeast is 3.0Á5.0 and that they can also grow well at neutral pH range. Our research results showed the positive correlation between pH and yeasts, although Vreulink et al (2007) found in their study on sandy soil that the correlation between soil pH and culturable soil yeast numbers is negative and Moawad et al (1986) observed no significant effect at all.…”
Section: Soil Phcontrasting
confidence: 70%
“…Conversely, it is well known that the optimum growth pH range for yeast is 3.0Á5.0 and that they can also grow well at neutral pH range. Our research results showed the positive correlation between pH and yeasts, although Vreulink et al (2007) found in their study on sandy soil that the correlation between soil pH and culturable soil yeast numbers is negative and Moawad et al (1986) observed no significant effect at all.…”
Section: Soil Phcontrasting
confidence: 70%
“…The choice of sugar beet as a host was intentional in the expectation that a plant high in sugar reserves would be an attractive niche for yeasts in general. Earlier reports have indicated dominance of yeasts on fruits (Wilson and Wisniewski 1989; Filonow 1998) and roots rich in sugars (Babeva and Belyanin 1966; Moawad et al. 1986).…”
Section: Discussionmentioning
confidence: 94%
“…Some of these genera, such as Aureobasidium and Trichosporon, can also have mycelial phases (Barnett et al 1990). Moawad et al (1986) reported that population densities of yeast in soils correlated significantly with the organic carbon and organic nitrogen content of soils tested. di Menna (1962) concluded, from qualitative and quantitative surveys of the yeast flora of New Zealand soils, that yeast populations varied qualitatively from place to place with soil type and vegetation but not with season, whereas the density of yeast populations was different from place to place and also varied with season.…”
Section: Introductionmentioning
confidence: 98%
“…Bab'eva and Belyanin (1966) found the colony-forming units of yeasts in the rhizosphere of cabbage, corn, sugar beet, and oats to be higher compared to normal bulk soils. Not only were the number of yeasts higher in the rhizosphere, but also the species compositions were more diverse (Bab'eva and Belyanin 1966;Moawad et al 1986). …”
Section: Introductionmentioning
confidence: 99%