Doctoral Dissertation Soil fertility and its correlation with green-tea elemental and functional components in a special tea-production area around Cong River in Thai Nguyen province, Vietnam ベトナム国タイグエン省コン川沿いの 特産茶葉生産地における土壌肥沃度と その茶葉成分への影響に関する研究 by Hoang Huu Chien Kuroshio Science program Kochi University March 2020 Contents Summary. Tea plant and its production and consumption in Vietnam. Chemical components related to tea quality. Tea garden soil and its interaction with tea production and tea quality.
Environmental and nutrient requirements of tea plantation. Soil acidification due to excessive N fertilization. Influence of soil acidification on soil-plant nutrient dynamics. Description of study area and sampling sites.
General information on Thai Nguyen province. Soil pedological characteristics of tea gardens. Materials and methods. Soil sampling and analysis.
Soil total elements. Si, Al, and Fe oxide-hydroxides and clay mineralogical composition. Soil characteristics in terms of mineralogy and weathering status. Soil chemical characteristics and fertility.
Assessment of soil fertility. Materials and methods. Soil sampling and analysis. Soil solution sampling and analysis.
Soil physicochemical properties. Trace elements availability. Soil physical properties. Chemistry of soil solution.
Characteristics of soils in the study area. Relevant factors to determine soil fertility status. Soil solution and leaching loss of nutrients from soils. Evaluation of tea quality.
Materials and methods. Tea leaves sampling. Functional components and tea evaluation. Importance of mineral elements.
Elucidation of important soil parameters affecting tea quality. Materials and methods. Results and discussion. Important soil parameters affecting tea quality.
Soil condition and the accumulation of nutrient elements in tea leaves. Conclusion and recommendation. 91 List of Tables Table 1. Tea production in the world and in Vietnam from 1970 to 2016.
Climatic condition of major tea production areas in Japan, China, India, and Vietnam. Information of study sites. Morphological properties of soils. Physicochemical properties of soils.
The contents of total elements in soils. Si, Al, and Fe oxide-hydroxides and clay mineralogical composition of soils. General physicochemical properties of tea garden soils in Tan Cuong commune. Comparison soil physicochemical properties between tea garden sites and forested sites on Transect B.
Comparison soil physicochemical properties of tea soils between Tan Cuong and Song Cau communes. The contents of potentially available Mn, Fe, Cu, and Zn in tea soils in Tan Cuong commune. Comparison of DTPA-extractable trace element contents in tea soils between Tan Cuong and Song Cau communes. Soil physical properties under tea gardens and forested patches in Tan Cuong commune.
Comparison of soil physical properties between Tan Cuong and Song Cau communes. Weighted averages of chemical properties of soil solutions under tea gardens in Tan Cuong commune. Critical contents of trace elements in soils. Correlation coefficients between DTPA-extractable trace elements and clay content, pH, and T-C in soils in Tan Cuong commune.
The contents of chemical components in tea leaves and tea infusion in Tan Cuong commune. Comparison of chemical components in tea leaves and tea infusions between Tan Cuong and Song Cau commnunes. Pearson correlation coefficients between the levels of functional components in tea infusions and those of mineral elements in tea leaves. Soil physicochemical properties in Tan Cuong and Song Cau communes used in regression analysis.
Multiple regression analysis of antioxidant activity, total polyphenols, and Catechins. Correlation between selected soil parameters and the contents of mineral elements in tea leaves. 83 List of Figures Fig 1. Tea export ranking in the world in 2016.
Thai Nguyen province in Northern region of Vietnam. Mean monthly temperature and precipitation in Thai Nguyen province in the period 2007-2017. Study area, transect lines and sampling sites in Tan Cuong and Song Cau communes. XRD patterns of the <2 µm clay fraction of selected soil samples.
The results of the PCA on total element composition of soils. Particle size distribution of tea garden soils at the surface 0-10 cm. Water retention curves of the soils. Seasonal fluctuation of soil solution chemistry.
Comparison of ion concentrations in soil solutions between two seasons at each sampling site. Relationship of T-C and T-N with garden age in Tan Cuong commune. Comparison of exchangeable bases, available P, NH4-N, and NO3-N between the depths of 0-10 cm and 20-30 cm in Tan Cuong commune. The results of the PCA on chemical components of tea leaves and tea infusion.
Grouping tea gardens based on the concentrations of Catechins, Theanine, total polyphenols, and antioxidant activity in tea infusions. Correlation between and theanine, total catechins, total polyphenols, and antioxidant activity in Trung Du tea infusions and tea farm-gate shipping prices. Correlations between clay contents and tea farm-gate shipping prices of tea in Tan Cuong commune. 84 List of main papers Main papers used in creating the dissertation Peer-reviewed papers 1.
Hoang Huu Chien, Maho Tokuda, Dang Van Minh, Yumei Kang, Kozo Iwasaki and Sota Tanaka (2019). Soil physicochemical properties in a high-quality tea production area of Thai Nguyen province in northern region, Vietnam. Soil Science and Plant Nutrition, 65 (1): 73- 81. Hoang Huu Chien, Dang Van Minh, Kozo Iwasaki and Sota Tanaka (2020).
Soil Morphological, Mineralogical and Chemical Characteristics of Tea Gardens with High- Quality Leave Production in Thai Nguyen province, Vietnam. Hoang Huu Chien, Sota Tanaka, Kozo Iwasaki, and Dang Van Minh. Evaluation of soil environment under tea gardens in special tea production area of Vietnam. 11th International Kuroshio Science Symposium, 25 July 2017.
Hoang Huu Chien, Maho Tokuda, Dang Van Minh, Yumei Kang, Kozo Iwasaki, and Sota Tanaka. Soil chemical properties in a high quality-tea production area of Thai Nguyen province, Vietnam. 10th International Symposium on Plant-Soil Interactions at Low pH, 25- 28 June 2018. 大友理佐，奥村夏帆 山根佳奈，Hoang Huu Chien, Dang Van Minh, 島村智子, 田中 壮太, 岩崎貢三.ベトナム北部タイグエン省の茶園で栽培された茶葉の品質と茶園土 壌の性質.日本土壌肥料学会2019年度静岡大会.
Soil Properties Affecting the Quality of Special Local Tea Produced in Thai Nguyen Province, Northern Vietnam. 14th International Conference of the East and Southeast Asia Federation of Soil Science Societies. In Vietnam, green tea is one of the most favorite beverage and tea production plays an important role in the national agricultural sectors. Tan Cuong commune in Thai Nguyen province is considered as the core center of tea production with special tea quality.
The evaluation of tea products by the stakeholders varied within the commune, which is usually higher for the tea leaves produced around the riverside of Cong River than those away from. It could be assumed that such difference in tea evaluation may result from the differences in soil environments due to topographic or other conditions in the commune. Meanwhile, it is believed that increasing N uptake from soil brings about the increase both in the yield and quality of tea plants, particularly the content of Theanine, which is determinant for the “umami” and fragrance of tea infusion. Because of this, excessive N fertilizer is applied, which may cause excessive soil acidification, the leaching loss of nutrient elements, and water pollution.
However, the information on tea garden soils has been quite limited in Vietnam. The purposes of this study are to investigate the soils in terms of the distance from Cong River and to correlate the soil factors with the contents of elemental components and functional components in tea leaves including Theanine as well as Catechins (polyphenols; responsible for bitter and astringent taste with a function of antioxidant effect) in order to develop appropriate, environmental-friendly soil management schemes for tea production. Materials and methods: The study area was located in the flood plain of Cong River in Tan Cuong. The terrain was composed of back marsh lowland with interspersing rows of the current natural dike and, followed by river terraces away from the river.
Tea gardens were located on the lowlands adjacent to the river and on the previous dikes or hill slopes. Three transect lines (A, B, and C) were installed perpendicularly to the river, each on which four study sites were established. They were coded as A1 to A4, B1 to B4, and C1 to C4. For comparison, four forested patches adjacent to the tea gardens on transect B 1 (BF1, BF2, BF3, and BF4) were selected.
In addition, three tea gardens were studied in Song Cau (S1, S2, and S3) which was considered as the inferior tea production area. For pedological characterization, soil profiles were described at B1 to B4 and S1 and soil samples were collected from each pedological horizon for general physicochemical analysis, clay mineral composition, Al, Fe and Si oxide-hydroxides, and total element contents. To assess soil fertility, soil samples were collected at the depth of 0-10 cm and 20-30 cm in all study sites and analyzed for general physicochemical properties and DTPA-extractable contents of Mn, Fe, Cu, and Zn. Undisturbed soil samples were collected at the depths of 0-10 cm and 20-30 cm in B1 to B3, BF1, BF3, and S1 sites to assess soil physical properties.
At B1 to B4, soil solution was weekly collected at 20 cm depth and its chemistry was analyzed. Meanwhile, tea leaf samples were collected for the total element analysis. For tea infusion by boiling water, the contents of total elements and the concentrations functional components (Theanine, Catechins, total polyphenols, and antioxidant activity) were determined. Although all soils were strongly acidic throughout the profile with high contents of exchangeable Al, pedological characteristics varied, depending on physiological location of tea gardens and soil disturbance: the B1 and BF1 soils at the riverside were classified as Typic Ustipsaments.
They were deep, sandy- textured, and predominated by quartz and kaolin minerals in the clay fraction. Meanwhile, the B2 to B4 and BF3 soils far from the river were Typic Dystrustepts while the S1 soil was Typic Paleustults. These soils were relatively shallow, fine-textured with 2:1 clay minerals as well as kaolin minerals. The (Fed-Feo)/Fet ratio was the lowest in B1 and BF1 sites and the highest in S1 site.
These results indicated that the former soils were supplied as sediments upon flooding while the latter were intrinsic in relatively moderate - weathered status. The analysis of total element contents supports these views. In addition, the influences of soil disturbance were observed in the soil profiles and properties in B2 and B4 sites. The soils showed strongly acidic nature with the average pH(H 2O) of 3.7 at the surface and 3.9 at the subsurface.
The ECEC was low, and dominated by exchangeable Al. In spite of such acidic condition, a relatively large saturation of exchangeable Ca, K, and Mg on the ECEC was found in the surface soils. The level of available P was high, occasionally exceeding 1000 and 500 mg kg -1 at the surface and subsurface, respectively. Nitrification was not restricted, and a portion of NH4-N applied as fertilizers was converted to NO3-N in the surface soils to move down to deeper layers.
Three determinant factors of soil properties and fertility were identified: the first is the distance from the river for which soil texture classes varied from sandy loam close to the river to light clay far from the river. Physical properties were related to soil texture and also depended on the distance from the river. Influences on these properties by soil compaction were found at the riverside site. In addition, the exposure of subsurface soils due to severe disturbance was found in the farthest site from the river.
The second was the garden age for which the levels of T-C and T-N were correlated with increasing age, suggesting that the addition of plant residue and manure replenished soil organic matter pools after the establishment of tea gardens. Lastly, fertilizer management practices principally determined the levels of the exchangeable bases, available P, and mineral N. However, a significant portion of these nutrients was likely to exist in water soluble forms without adsorption onto soils.