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§ Fertilizers and nutrients:
被覆燐硝安加里(ロング・ハイコントロール・Nutricote)の特性について(その2)
Shibata Professional Engineers Office
柴田 勝
§ Soil and fertilizer management to improve soil fertility in tea plantation soils
Jcam Agri Corporation Kyushu Branch
郡司掛 則昭
Shibata Professional Engineers Office
柴田 勝
In view of the impact of agriculture on the environment, soil fertilizer technology has been compiled as the basis for harmonizing the environment and productivity. The simplification of soil diagnostic techniques and the practical application of software that calculates the appropriate amount of fertilizer based on the data collected have helped to optimize the use of fertilizers. In addition, the use of fertilizer with a high nutrient utilization rate and controlled fertilizer application is recommended as a measure to reduce the impact of nitrate-form chisso on water quality. In this context, coated fertilizers, which can supply nutrients in accordance with crop growth (nutrient absorption), have become well understood and are used for many crops as a typical fertilizer with regulated fertilizer use that harmonizes productivity and the environment (Figure 5).

Coated fertilizers are characterized by their ability to supply nutrients in proportion to the amount of nutrients absorbed by the crop and to reduce losses due to runoff, as well as by their well-controlled leaching, which makes it possible to apply fertilizers in a base fertilizer-intensive system. Coated fertilizers are base fertilizers in terms of application timing, but their function is that of a supplementary fertilizer. The coated fertilizers are applied together with the base fertilizer, which logically reduces the amount of additional fertilizer, and the base fertilizer-intensive fertilization method has taken root, harmonizing the environment and productivity.
The revolutionary fertilizer application method brought about by coated fertilizers is the root zone fertilization method. Conventional fertilizers are usually applied in a full layer or intentionally at a distance from the roots, because fertilizer components cause concentration disturbance to the roots and significantly inhibit growth when applied close to the roots. Coated fertilizers supply nutrients according to the amount absorbed by the crop, so they do not cause concentration disorders such as root scorching, and can be applied close to the roots, resulting in improved nutrient utilization and reduced fertilizer application. The nutrient for which harmony with the environment is most needed is the thioester component, and the advent of coated fertilizers has made it possible to optimize (reduce) the amount of thioester fertilizer applied (Figure 6).


Table 4 summarizes the adaptability of fertilizer application methods and fertilizers. Fertilizer application location is closely related to nutrient utilization; the closer the fertilizer is to the roots, the higher the utilization, but on the other hand, there are concerns about root damage. Coated fertilizers with excellent leaching control performance enable local application of fertilizers in planting holes, in pots, and by contact, which could not be achieved with synthetic slow-release fertilizers.

Coated fertilizers can also be defined as fertilizers that can significantly increase the amount of fertilizer applied relative to the soil volume. Polyolefin resin-coated fertilizers, in particular, have high leaching control performance and do not cause root scorch, enabling the practical application of these new fertilization methods. The cultivation method using localized fertilization, which has developed in place of the full-layer fertilization method, can be called root-area controlled cultivation. The total box fertilization of rice seedlings using LP coat, coated fertilizers, and "seedling box leave" is the ultimate example of such a method. In the horticultural field, various root zone control methods are actually used, such as isolated bed cultivation in greenhouses, mulch film-covered cultivation, elevated strawberry cultivation, and container cultivation of fruit trees, and the use of coated fertilizers is expanding.
One thing to keep in mind when using root zone control cultivation with coated fertilizers is that since the amount of soil per fertilizer is reduced, it is necessary to consider how to deal with the reduced nitrification capacity of the soil. In the case of cultivation methods using artificial media such as coconut fiber or rockwool, the nitrification capacity is even smaller than in soil cultivation. Particularly, when coated urea is applied to the root zone, the nitrification potential of the root zone should be taken into consideration. When cultivating horticultural crops with a high amount of nitrogen fertilizer in the root zone, it is preferable to use a coated fertilizer containing nitrate-form nitrogen that is supplied continuously and systematically. It would be a waste if the roots of the crop are damaged.
Most of the brands of coated compound fertilizers in Japan and around the world are based on NPK compound fertilizers containing nitrate-form chisso, and the distribution of coated compound fertilizers based on ammonia-based compound fertilizers is unheard of.
Ammonium nitrate is a water-soluble fertilizer containing 351 TP3T of water-soluble chisso (17.51 TP3T each of ammonia- and nitrate-form chisso), and is considered to be a raw material for coating fertilizer as well as urea containing 461 TP3T of water-soluble chisso, but the risk of explosion increases when ammonium nitrate and organic matter coexist, making ammonium nitrate However, the coexistence of ammonium nitrate and organic matter increases the risk of explosion, making ammonium nitrate alone inappropriate. The addition of phosphoric acid and potassium eliminates this risk, so the granular raw material for coated fertilizers containing nitrate-form nitrate is a compound fertilizer with a nitrate complex NPK composition. Of course, the safety of each brand of coated fertilizer products has also been confirmed.
硝酸態チッソを含む被覆複合が示す,もっとも重要な特長は「肥料に対する根の応答」(写真3)が物語っている。写真3は,チッソ成分量として5gの試験肥料を下部に入れ,肥料分を含まない土壌で封をしたφ3cm×12cmの紙筒パイルをトマト苗を定植した根箱に差し込み,トマトを生育させて,根箱側面から根の伸展を撮影した試験結果である。使用した肥料は「くみあい燐硝安加里S555」 ,被覆燐硝安加里「ロング424−70タイプ」 ,被覆尿素「LPコート70タイプ」である。

As shown in Photo 3 (left), plant roots are thought to grow by sensing the presence of nutrients through EC (electrical conductivity), but root extension is affected by the type and concentration of nutrients present in the soil. As shown in the right side of Photo 3, in the phosphonitrite-alkali area, the nutrient concentration is high just below the paper tube, so the roots spread out as if they were receiving nutrients at a little distance from the bottom of the paper tube. In the urea-phosphorus-coated long 424-70 type, the amount of roots around the paper tube was high, and white roots were surrounding the paper tube as if they were swarming around it. The inactive root elongation in the urea-coated zone is assumed to be due to a failure of nitrification of ammonia produced by the decomposition of urea, which is caused by the accumulation of ammonia. Caution should be exercised when using coated urea in root zone controlled cultivation of horticultural crops with high fertilizer application.
カルシウム(ホウ素も)を欠除すると劇的に根の伸長が停止することが知られている(図7) 。カルシウム(ホウ素も)は細胞壁の形成に重要な役割を果たしており,根の伸長のためにはカルシウムの吸収は欠かせない。硝酸態チッソはカルシウムの吸収を促進することが知られており(表5),ロング区のすぐれた根の伸展はカルシウムを吸収促進させている結果であろうと推察される。ロングは健全な根の成長を促す肥料でもある。


Nitrate-form chisso is an essential nutrient for horticultural crops, but nitrate ions are not easily adsorbed by the soil, so they are easily transported to the subsoil layer of the field through subsurface infiltration of rainwater. The significance of nitrate-form nitrate cover is to increase the efficiency of nitrate-form nitrate utilization by continuously absorbing nitrate-form nitrate, which is an important nutrient for crops. The significance of nitrate-form chisso coverage is summarized in Table 6.

Jcam Agri Corporation Kyushu Branch
郡司掛 則昭
Tea production in Kagoshima Prefecture is thriving, with tea plantation area of 7,990 ha and rough tea production of 28,100 t in 2018, both second in Japan. However, the current state of soil fertility in tea plantation soils has been pointed out to have problems mainly in chemistry, such as low pH, accumulation of phosphoric acid and potassium, and nutrient imbalance.
Low pH is particularly serious. Tea is a crop that prefers a low soil pH, and low pH itself is not so much of a problem. However, it has been reported that tea growth and yield are affected when pH 4 or lower is strongly acidic, because the amount of fine roots that absorb nutrients in the tea plant decreases and its fertilizer absorption capacity decreases (Nonaka, 2005). On the other hand, as a result of the long-standing practice of high-fertilizer cultivation in tea plantations for high yield and quality improvement, the accumulation of fertilized phosphoric acid and potassium in the soil tends to become apparent, and improved fertilizer application is required to reduce the accumulation.
Here, as a continuation of the article "Actual Soil Fitness and Soil Preparation of Kagoshima Prefecture Tea Plantation Soils" published in the May 2017 issue of the same journal, we would like to discuss specific measures for soil and fertilizer management to solve soil fertility problems such as low pH, phosphoric acid and potassium accumulation that tea plantation soils are facing.
According to recent soil diagnostic results on Kagoshima Prefecture tea garden soils (Nagata, 2019), pH averaged 3.5, well below the diagnostic standard value of 4 to 5 (Table 1).

EC averaged 0.6 mS/cm, exchangeable calcium and magnesium averaged 97 mg and 38 mg, respectively, which were within the appropriate range of soil diagnostic criteria, while exchangeable potassium averaged 49 mg, which was higher than the diagnostic criteria. Base saturation and lime saturation were 25% and 13%, respectively, which were almost equal to or less than the lower limit of the diagnostic criteria, while lime/bittern ratio and bittern/potassium ratio, which indicate nutrient balance, were both 1.9, which were below the standard values. The lime/bituminous soil ratio was particularly high. The average value of dietary phosphoric acid was 137 mg, more than twice the upper limit of the diagnostic criteria (50 mg).
Thus, the current state of soil fertility in tea plantations is mainly due to chemical problems such as low pH, phosphate and potassium accumulation, and nutrient imbalance. The most effective countermeasures are acidity correction by applying calcareous materials to raise pH and reducing fertilizer to prevent the accumulation of phosphate and potassium nutrients. The nutrient imbalance can be corrected by correcting the acidity and reducing the amount of fertilizer.
One of the reasons for the decrease in soil pH is that the tea plantation soils are black granite soil. Black granite soil is composed of volcanic ash, which contains a large amount of active aluminum, which is hydrolyzed to release hydrogen ions and acidify the soil. However, this aluminum hydrolysis reaction alone does not reduce the pH below 4. In addition, other nutrient conditions, such as low exchangeable calcium and high concentrations of soluble phosphate, are thought to be deeply involved in lowering the pH.
A graphical representation of the relationship between pH and other chemical properties for the 436 Kagoshima Prefecture tea garden soils introduced in the May 2017 issue of the same journal shows that pH decreases as exchangeable potassium and salable phosphate increase, but conversely increases for exchangeable calcium or magnesium (Figure 1). However, since it is difficult to determine the percentage contribution of each chemical property to the increase or decrease in pH from the graph, we performed a multiple regression analysis with pH as the objective variable and the other chemical properties as explanatory variables, resulting in the following multiple regression equation.
pH = -0.62*** x EC + 0.0032*** x exchangeable calcium - 0.0032*** x ratable phosphate + 4.05
Here the coefficient of determination R2 = 0.80, and an asterisk (**) in each partial regression coefficient indicates that it is statistically significant at the 11-TP3T level.

From this multiple regression equation, it is clear that EC, exchangeable calcium, and free-form phosphate are the chemistries that contribute significantly to pH change. Furthermore, when the analytical values of these three chemistries varied within the range of minimum to maximum values (Table 1, Fig. 2), the pH did not reach the lower limit of the diagnostic standard value, 4.0, even when the analytical values of EC and exchangeable phosphate reached the minimum, but increased to 4.0, which is within the diagnostic standard value, when the amount of exchangeable calcium increased to about 250 mg However, when exchangeable calcium is increased to about 250 mg, the pH level rises to 4.0, which is within the diagnostic standard. Therefore, it can be inferred that increasing exchangeable calcium is the simplest and most effective method of acidity correction.


(2002) reported that the target pH for acidity correction is 4.5 because the retention of ammonia nitrogen, which is important for tea tree growth, is unexpectedly low in the pH range of 4 to 4.4 and is easily leached out. Based on this, the target pH was set at 4.5. Based on this, the amount of calcareous material (calcium carbonate) required when the target pH is set at 4.5 was determined by the following procedure using multiple regression equations.
(1) Find the exchangeable calcium content at the current pH of 3.47 from the multiple regression equation (= 87 mg)
(ii) Find the exchangeable calcium content at target pH 4.50 from multiple regression equation (= 418 mg)
(3) Subtract (1) from (2) to obtain the amount of exchangeable calcium required for acidity correction (= 331 mg)
(iv) Convert the amount of exchangeable calcium into the amount of calcareous material applied (charcoal calcium) (= 591 mg)
Here, the average values of soil depth and provisional specific gravity of Kagoshima Prefecture tea garden soils are 13 cm and 0.66, respectively (Kyushu Agricultural Administration Bureau, 2010), and if the ridge area is 1/5 of the tea garden area, this 591 mg is equivalent to about 100 kg of calcium carbonate per 10 a. The average values of soil depth and provisional specific gravity of the Kagoshima Prefecture tea garden soils are 13 cm and 0.66, respectively (Kyushu Agricultural Administration Bureau, 2010).
The amount of calcium carbonate applied at about 100 kg/10a is almost equivalent to the amount of calcareous materials commonly applied for soil management in black box tea plantations, and the estimation of the amount of calcareous materials applied by the multiple regression equation here seems reasonable.
In the section 2, "Current status of soil fertility in tea plantations," it was pointed out that phosphoric acid and potassium are accumulated in tea plantations, and this is well recognized not only by the prefecture but also by JA and other organizations. However, it is not clear whether these reduced fertilizer standards provide sufficient nutrients for tea plant growth, so we examined the annual nutrient balance of phosphoric acid and potassium to verify the validity of the current standards.

茶樹によるリン酸あるいはカリの養分収支を正確に測定することは容易ではないが,既に明らかにされている窒素収支モデル(鹿児島農総セ2006)に基づいてリン酸あるいはカリの収支を推定することは可能である。推定方法は,施肥窒素の茶葉や整せん枝葉による吸収量や土壌中養分濃度への分配割合を示す窒素収支モデルを基にリン酸およびカリを案分して求めるものである。仮定としては,
①施肥したリン酸およびカリの利用率はそれぞれ20%および50%とする,
②リン酸およびカリの土壌中濃度は分析値mg/100gに仮比重0.75を掛けてkg/10aに換算する,
③リン酸溶脱量はゼロとする,
④カリ溶脱量は黒ボク畑地での作土からのカリ溶脱量から推定する(野口,2015)
などである。
According to the annual balance of phosphoric acid and potassium determined in this way, if the prefectural fertilizer standard is followed (Figure 3), a fertilizer application of 24 kg of phosphoric acid would result in a balance of +16 kg of phosphoric acid and an estimated increase of 151 TP3T per year from the current 104 kg/10a to 120 kg/10a of soluble phosphoric acid. On the other hand, the annual balance of potash will be +8 kg, and exchangeable potassium, which is currently 42 kg/10a, will increase by 191 TP3T to 50 kg/10a. Therefore, fertilization according to the prefectural standard for both phosphate and potassium will increase the current concentration of nutrients in the soil and cannot be used as a measure to prevent accumulation.

In contrast, if the JA standard is followed (Fig. 4), the annual balance with 13 kg of phosphoric acid fertilizer is +5 kg, and the annual increase in edible phosphoric acid is 51 TP3T from 104 kg/10a to 109 kg/10a, so it is assumed that further fertilizer reduction is necessary because the current JA standard cannot prevent accumulation.
On the other hand, the balance of potassium is -4 kg after 7 kg of fertilizer, which is the JA standard, and -9 kg after adding leaching, resulting in an annual balance decrease of 211 TP3T, which can prevent potassium accumulation. However, potassium decreases as much as 211 TP3T per year, and if this process is repeated, potassium is estimated to be below the soil diagnostic standard after 2 or 3 years. Therefore, it is recommended that the potassium level be set higher than the current fertilizer standard.

As summarized in Table 3, the annual nutrient balance of phosphoric acid and potassium suggests that fertilization with phosphoric acid according to the current JA standards would not avoid accumulation due to an increase in ratable phosphoric acid, and that fertilization with potassium would cause a rapid decrease in exchangeable potassium and could lead to a drop below the diagnostic standard. For these reasons, it is necessary to change the current standards, and to prevent accumulation of phosphoric acid and potassium while slowly decreasing the amount of accumulated nutrients, we propose a change to 6 kg of phosphoric acid, which is roughly half the current standard, and a change to 14 kg of potassium, which is twice the current standard.
The annual balance of phosphoric acid and potassium in this proposal (Fig. 5, Table 3) is -2 kg and -2 kg, respectively, even if 5 kg of leaching is taken into account, and the concentrations of both phosphoric acid and potassium in the soil decrease slowly to prevent accumulation. Therefore, it seems to be effective as a proposal to reduce phosphate and potassium fertilizers.


The current state of soil chemistry in Kagoshima Prefecture tea gardens is characterized by extremely low pH, soil accumulation of phosphate and potassium, and nutrient imbalance, suggesting the need for soil and fertilizer management that can quickly resolve these soil fertility problems.
Among these, a significant decrease in pH affects nitrogen absorption and leaching, which are the most important factors for tea plant growth and quality, so optimization of pH is an urgent issue. Therefore, multiple regression analysis of tea garden soil chemistry has shown that exchangeable calcium, EC, and edible phosphate contribute significantly to pH fluctuations, and that soil management that increases exchangeable calcium is the most effective way to raise pH. It was inferred that the application of about 100 kg/10a of calcareous material (calcium carbonate) per year to correct acidity is appropriate.
It is difficult to prevent soil accumulation of phosphoric acid and potassium with the current JA standards, and in particular, a rapid decline in potassium was observed, so it was decided that the current standards should be changed. The proposed changes include increasing phosphoric acid fertilizer to 6 kg/10a, about half the current standard, and doubling the amount of potash to 14 kg, which would slowly prevent accumulation. It will be necessary to conduct a field demonstration to verify the validity of the proposed changes.
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