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Factors influencing the Se content in tea leaves and rhizosphere soils of the Liubao tea in Wuzhou City, Guangxi |
PENG Xue-Rui( ), CHEN Xiang, ZHOU Si-Yu |
No. 270 Geological Team of Guangxi Zhuang Autonomous Region, Liuzhou 545005, China |
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Abstract This study aims to investigate the characteristics and influencing factors of selenium (Se) content in the tea leaf-rhizosphere soil system of the Liubao tea in Wuzhou, Guangxi. With the main tea gardens in Liubao and Shizhai towns, the core production areas of the Liubao tea, as study areas, this study conducted statistical analysis of the Se content in the tea leaves, rhizosphere soils, and tea leachate samples of the Liubao tea. The results show that: ① The Se content in soils of the study areas ranged from (0.40~1.98)×10-6, averaging 1.08×10-6; ② The Se content in Liubao tea leaves was between (0.03~0.25)×10-6, averaging 0.07×10-6, with a Se enrichment rate of 68%; ③ The leaching rates of Se in tea leachate ranged from 0~23.95%; ④ The Se content in the rhizosphere soils of tea gardens principally depended on soil parent materials and silica-sesquioxide ratios; ⑤ The P and N elements in soils can facilitate the absorption of soil Se by tea leaves, while the iron and aluminum oxides in acidified soils hinder the full utilization of soil Se by the Liubao tea. Hence, appropriate biochemical and agronomic measures are recommended for acidified soil amelioration to enhance the Se enrichment ability of the Liubao tea.
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Received: 20 January 2023
Published: 16 April 2024
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Sampling points in study area
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指标 | 标准偏差 | 变异系数 | 最大值 | 最小值 | 平均值 | 浓集系数(K) | Al2O3 | 2.74 | 0.16 | 23.03 | 10.96 | 16.84 | 1.34 | CaO | 0.02 | 0.24 | 0.15 | 0.054 | 0.08 | 0.03 | Corg | 0.29 | 0.21 | 2.17 | 0.87 | 1.39 | 3.97 | Fe2O3 | 1.51 | 0.24 | 9.51 | 2.93 | 6.36 | 1.35 | K2O | 0.34 | 0.17 | 2.80 | 1.29 | 2.07 | 0.83 | MgO | 0.09 | 0.14 | 0.86 | 0.47 | 0.65 | 0.36 | SiO2 | 5.61 | 0.09 | 77.57 | 51.53 | 63.66 | 0.98 | As | 13.25 | 0.56 | 72.50 | 7.07 | 23.60 | 2.36 | B | 13.32 | 0.32 | 78.70 | 9.93 | 41.49 | 1.04 | Cd | 0.07 | 1.06 | 0.50 | 0.013 | 0.07 | 0.78 | Cr | 20.59 | 0.21 | 150.00 | 58.90 | 95.81 | 1.47 | Cu | 4.62 | 0.18 | 39.10 | 19.20 | 26.30 | 1.10 | Ge | 0.20 | 0.14 | 1.74 | 0.70 | 1.38 | 1.06 | Hg | 0.04 | 0.38 | 0.27 | 0.061 | 0.11 | 2.75 | Mn | 95.57 | 0.65 | 488.00 | 56.50 | 147.19 | 0.25 | Mo | 1.44 | 0.76 | 7.60 | 0.50 | 1.90 | 2.38 | N | 243.68 | 0.19 | 2092.00 | 872.00 | 1283.66 | 2.01 | Ni | 4.55 | 0.20 | 37.90 | 11.20 | 22.87 | 0.88 | P | 105.47 | 0.27 | 700.00 | 235.00 | 389.08 | 0.75 | Pb | 6.21 | 0.21 | 51.10 | 20.30 | 28.92 | 1.26 | S | 69.14 | 0.24 | 472.00 | 157.00 | 288.00 | 1.92 | Se | 0.44 | 0.41 | 1.98 | 0.40 | 1.08 | 5.40 | Ti | 635.45 | 0.12 | 7213.00 | 4071.00 | 5094.82 | 1.18 | Zn | 10.92 | 0.27 | 68.00 | 22.00 | 40.21 | 0.59 | pH值 | 0.25 | 0.06 | 5.12 | 3.96 | 4.41 | | Saf | 0.85 | 0.29 | 5.58 | 1.58 | 2.89 | 0.41 |
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Characteristics of parameter contents in rhizosphere soils of Liubao tea of the study area(n=50)
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| 洞口组一 段($\epsilon$h1) | 洞口组二 段($\epsilon$h2) | 黄洞口组 三段($\epsilon$h3) | 小内冲组 ($\epsilon$x) | τ | 1.18 | 0.40 | 0.23 | 5.16 |
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Statistics of mass transfer coefficient of selenium in different geological background(n=40)
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Contents of selenium along vertical soil profiles of different geological backgrounds
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指标 | r | | 指标 | r | | 指标 | r | | 指标 | r | Cr | 0.884** | | As | 0.313* | | Corg | 0.016 | | N | -0.148 | Ti | 0.793** | | Cu | 0.307* | | K2O | -0.015 | | Pb | -0.158 | Mo | 0.560** | | Saf | -0.785** | | B | -0.018 | | Zn | 0.161 | Ni | 0.499** | | P | -0.370** | | Cd | -0.124 | | pH | -0.022 | Ge | 0.460** | | S | -0.327* | | Hg | -0.150 | | | | MgO | 0.428** | | CaO | -0.042 | | Mn | -0.106 | | | |
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Correlation coefficients of selenium contents and other physicochemical parameters of rhizosphere soils (n=50)
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样品序号 | 茶叶中Se 含量/10-6 | 浸出液中Se 浓度/(mg·L-1) | 浸出率/% | 1 | 0.074 | 0.0005 | 13.51 | 2 | 0.130 | 0.001 | 15.38 | 3 | 0.248 | 0.001 | 8.06 | 4 | 0.084 | 0.001 | 23.95 | 5 | 0.062 | 0 | 0 | 6 | 0.082 | 0 | 0 |
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Dissovled rate of selenium in tea
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指标 | r | 指标 | r | 指标 | r | Saf | 0.734** | Se | -0.686** | Ge | -0.317* | P | 0.546** | Cr | -0.596** | pH | 0.035 | N | 0.501** | As | -0.478** | Corg | 0.228 | S | 0.349* | Ti | -0.461** | | | Hg | 0.292* | MgO | -0.341* | | |
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Correlation coefficients between the bioconcentration factors of selenium in tea leaves and contents of other elements in soils(n=50)
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| n | Saf | Se土平均值 | Se茶平均值 | 相关系数 | A组 | 30 | 1.58~2.92 | 1.32 | 0.064 | 0.121 | B组 | 30 | 2.51~5.38 | 0.82 | 0.062 | 0.582** |
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Characteristics of selenium contents in rhizosphere soils and tea leaves of group A and group B
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Scattered plots of selenium contents in rhizosphere soils and tea leaves of group B
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