摘要
There is limited information on the pedological requirements of <i><span>Triumfetta cordifolia</span></i>. A starting point <span style="font-family:;" "="">for</span><span style="font-family:;" "=""> establishing such information requires knowledge on the growing environment of the species. The aim of this study was to <span>assess the physicochemical properties and mycorrhizal status in the rhizosphere of <i><span>Triumeffa cordifolia</span></i></span>. Soil and root samples from the rhizosphere </span>of <i><span>T. cordifolia</span></i> were collected from three localities (Santchou, Bandjoun<span style="font-family:;" "="">,</span><span style="font-family:;" "=""> and Balatchi) in the West Region of Cameroon. The results show that the soils are dominated by a loamy texture and have a mean porosity > 50%. Mean bulk density ranges from 0.91 ± 0.02 to 1.26 ± 0.04 g</span><span style="font-family:;" "=""><span style="white-space:nowrap;"><span style="white-space:nowrap;">⋅</span></span></span><span style="font-family:;" "="">cm<sup><span style="white-space:nowrap;"><span style="white-space:nowrap;">−</span></span>3</sup>. The sum of exchangeable cations ranges from medium (6.45 ± 1.02) to high (11.21 ± 1.35) and are evident of the satisfactory soil organic matter (OM) content in the various localities (5.90% ± 0.42% to 10.65% ± 0.73%). Total nitrogen (TN) content of the soils ranged from low (0.10%) to very high (0.41%). Biological activity is low due to very poor OM quality (mean C/N > 20). The average available phosphorus status ranged from medium (18.32 ± 3.91 ppm) to very high (69.39 ± 26.09 ppm). The Cationic Exchange Capacity (CEC) was moderate (19.28 - 29.28 cmol</span><span style="font-family:;" "=""><span style="white-space:nowrap;"><span style="white-space:nowrap;">⋅</span></span></span><span style="font-family:;" "="">kg<sup><span style="white-space:nowrap;"><span style="white-space:nowrap;">−</span></span>1</sup>) and was mainly contributed by soil organic matter. Base saturation ranged from low (28.0%) to medium (48.83%). Assessment of endomycorrhizal colonization showed that the intensity (I), frequency (Fr) and specific density of spores (Ds) were not significantly different among sites. A high level of available P in the Santchou soils appears to be the major cause for </span><span style="font-family:;" "="">the </span><span style="font-family:;" "="">lowest values of Fr, I</span><span style="font-family:;" "="">,</span><span style="font-family:;" "=""> and Ds observed. These results reaffirm the link between soil physicochemical properties and endomycorrhizal infection in <i><span>T. cordifolia</span></i></span>. Site characteristics and soil OM quality are factors to be considered in promoting the establishment of mycorrhizal symbiosis for profitable and sustainable cultivation of <i><span>T. cordifolia</span></i>.
There is limited information on the pedological requirements of <i><span>Triumfetta cordifolia</span></i>. A starting point <span style="font-family:;" "="">for</span><span style="font-family:;" "=""> establishing such information requires knowledge on the growing environment of the species. The aim of this study was to <span>assess the physicochemical properties and mycorrhizal status in the rhizosphere of <i><span>Triumeffa cordifolia</span></i></span>. Soil and root samples from the rhizosphere </span>of <i><span>T. cordifolia</span></i> were collected from three localities (Santchou, Bandjoun<span style="font-family:;" "="">,</span><span style="font-family:;" "=""> and Balatchi) in the West Region of Cameroon. The results show that the soils are dominated by a loamy texture and have a mean porosity > 50%. Mean bulk density ranges from 0.91 ± 0.02 to 1.26 ± 0.04 g</span><span style="font-family:;" "=""><span style="white-space:nowrap;"><span style="white-space:nowrap;">⋅</span></span></span><span style="font-family:;" "="">cm<sup><span style="white-space:nowrap;"><span style="white-space:nowrap;">−</span></span>3</sup>. The sum of exchangeable cations ranges from medium (6.45 ± 1.02) to high (11.21 ± 1.35) and are evident of the satisfactory soil organic matter (OM) content in the various localities (5.90% ± 0.42% to 10.65% ± 0.73%). Total nitrogen (TN) content of the soils ranged from low (0.10%) to very high (0.41%). Biological activity is low due to very poor OM quality (mean C/N > 20). The average available phosphorus status ranged from medium (18.32 ± 3.91 ppm) to very high (69.39 ± 26.09 ppm). The Cationic Exchange Capacity (CEC) was moderate (19.28 - 29.28 cmol</span><span style="font-family:;" "=""><span style="white-space:nowrap;"><span style="white-space:nowrap;">⋅</span></span></span><span style="font-family:;" "="">kg<sup><span style="white-space:nowrap;"><span style="white-space:nowrap;">−</span></span>1</sup>) and was mainly contributed by soil organic matter. Base saturation ranged from low (28.0%) to medium (48.83%). Assessment of endomycorrhizal colonization showed that the intensity (I), frequency (Fr) and specific density of spores (Ds) were not significantly different among sites. A high level of available P in the Santchou soils appears to be the major cause for </span><span style="font-family:;" "="">the </span><span style="font-family:;" "="">lowest values of Fr, I</span><span style="font-family:;" "="">,</span><span style="font-family:;" "=""> and Ds observed. These results reaffirm the link between soil physicochemical properties and endomycorrhizal infection in <i><span>T. cordifolia</span></i></span>. Site characteristics and soil OM quality are factors to be considered in promoting the establishment of mycorrhizal symbiosis for profitable and sustainable cultivation of <i><span>T. cordifolia</span></i>.
作者
Romary Tchinda Ngnipa
Fritz Oben Tabi
Souleymanou Adamou
Primus Azinwi Tamfuh
Georges Kogge Kome
Alexis Boukong
Antoine David Mvondo Ze
Romary Tchinda Ngnipa;Fritz Oben Tabi;Souleymanou Adamou;Primus Azinwi Tamfuh;Georges Kogge Kome;Alexis Boukong;Antoine David Mvondo Ze(Department of Soil Science, Faculty of Agronomy and Agricultural Sciences, University of Dschang, Dschang, Cameroon;Department of Agriculture, Faculty of Agronomy and Agricultural Sciences, University of Dschang, Dschang, Cameroon;Department of Mining and Mineral Engineering, National Higher Polytechnic Institute, University of Bamenda, Bambili, Cameroon)