1961
DOI: 10.1097/00010694-196109000-00005
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Relationships Between Ph Values of Organic Soils and Availabilities of 12 Plant Nutrients

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Cited by 210 publications
(129 citation statements)
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“…Organic soils are known to be acidic, minimalizing microbial decomposition and having high organic matter content with >30 C:N ratio immobilizing N; these are two characteristics that hinder N plant availability [44]. In our study, the organic soil was atypical with a pH of 7.7 and a C:N ratio of 15 that is ideal for N mineralization.…”
Section: Nitrogen Mineralization Occuring In Subarctic Cultivated Soilsmentioning
confidence: 78%
“…Organic soils are known to be acidic, minimalizing microbial decomposition and having high organic matter content with >30 C:N ratio immobilizing N; these are two characteristics that hinder N plant availability [44]. In our study, the organic soil was atypical with a pH of 7.7 and a C:N ratio of 15 that is ideal for N mineralization.…”
Section: Nitrogen Mineralization Occuring In Subarctic Cultivated Soilsmentioning
confidence: 78%
“…In a greenhouse experiment by Matsubara et al (2002), the soil pH of treatments receiving biochar increased from 5.4 to 6.2 (10% biochar by volume) and 6.3 (30% biochar by volume). According to Lucas and Davis (1961), these pH values fall within the pH range (5.5 to 7.0) where plant nutrients are near their maximum availability in agricultural soils. Many of these alterations in soil characteristics probably occur at a micro-scale , and thus may only affect hyphae that are in the immediate vicinity of biochar particles.…”
Section: Mechanism 1: Biochar Changes Soil Nutrient Availabilitymentioning
confidence: 98%
“…Additions of biochar to soil alters important soil chemical and physical (see below) properties such as pH (has caused both increases and decreases), and typically increase soil cation exchange capacity (CEC), and can lead to greater water holding capacity (WHC), while generally decreasing bulk density (Tryon 1948). Increases in soil pH towards neutral values (Lucas and Davis 1961), in addition to increased CEC (Glaser et al 2002), may result in increases in bio-available P and base cations in biochar influenced soils. Additionally, Lehmann et al (2003), Topoliantz et al (2005), Gundale and DeLuca (2006) and Yamato et al (2006) showed that biochar itself contained small amounts of nutrients that would be available to both soil biota (including mycorrhizal fungi) and plant roots.…”
Section: Mechanism 1: Biochar Changes Soil Nutrient Availabilitymentioning
confidence: 99%
“…All of the samples except two OFS sites (S-9 and S-10) represented the lower concentration of B in soil in all three cropping seasons ( Figure 10). The availability of increased concentration of B in OFS may be due to the continuous application of organic fertilizer in soil (Lucas and Davis, 1961).…”
Section: Resultsmentioning
confidence: 99%