scholarly journals Consecutive soybean (Glycine max) planting and covering improve acidified tea garden soil

PLoS ONE ◽  
2021 ◽  
Vol 16 (7) ◽  
pp. e0254502
Author(s):  
Shuilian Gao ◽  
Peng He ◽  
Tianxiu Lin ◽  
Haijuan Liu ◽  
Bin Guo ◽  
...  
Keyword(s):  
Glycine Max ◽  
Soil Ph ◽  
Cover Crop ◽  
Garden Soil ◽  
Organic Matters ◽  
Exchangeable Acidity ◽  
Exchangeable Bases ◽  
Exchangeable Al ◽  
Tea Garden ◽  
Different Parts

Planting soybeans (Glycine max (L.) Merr.) in tea gardens decreased soil pH in theory but increased it in practice. This controversy was addressed in this study by treating the tea garden soil consecutively with different parts of a soybean cover crop: aboveground soybean (ASB) parts, underground soybean (USB) root residues, and the whole soybean (WSB) plants. In comparison with the control, the soil pH increased significantly after the third ASB and WSB treatments, but there was no significant change in the soil pH in the USB treatment. Concordantly, the soil exchangeable acidity decreased significantly and the soil exchangeable bases increased significantly in the ASB and WSB treatments. The exchangeable acidity increased in the USB treatment, but the amount of the increased acidity was less than that of the increased bases in the ASB treatment, resulting in a net increase in the exchangeable bases in the WSB treatment. Soybean planting and covering also increased the microbial richness and abundance significantly, which led to significantly more soil organic matters. Exchangeable K+ and Mg2+, and soil organic matters played significantly positive roles and exchangeable Al3+ played negative roles in improving soil pH. Our data suggest that consecutive plantings of soybean cover crop increase the pH of the acidified tea garden soil.

scholarly journals Effect of Soil Acidity and Liming on Yields and Composition of Sugarcane Growing on an Ultisol

1969 ◽  
Vol 52 (2) ◽  
pp. 85-100
Author(s):  
Fernando Abruña Rodríguez ◽  
Juan Juárez ◽  
Raúl Pérez Escolar ◽  
José Vicente Chandler
Keyword(s):  
Soil Ph ◽  
Soil Acidity ◽  
Sucrose Content ◽  
Soil Factors ◽  
Base Content ◽  
Exchangeable Bases ◽  
Fertilized Soil ◽  
Exchangeable Al ◽  
Humid Region ◽  
Exchangeable Aluminum

Variable liming and heavy fertilization of a Cialitos clay (ultisol) over a 7-year period markedly affected soil properties and yields of subsequently planted sugarcane. A total of 3,680 pounds of N, 480 pounds of P, and 2,870 pounds of K had been applied per acre to all plots over this period. Cane yields increased from less than 1 ton per acre, when no lime had been applied, to over 40 tons when a total of 20 tons of limestone had been applied per acre over the previous 7-year period. Yields increased with increasing exchangeable base content in the upper 6 inches of soil from less than 10 tons per acre when exchangeable bases dropped below 3 meq., to over 40 tons when exchangeable bases exceeded 8 meq./l00 g. of soil (58-percent base saturation). Cane yields increased with decreasing exchangeable Al from less than 10 tons, when exchangeable Al exceeded 8 meq., to over 40 when exchange able Al was less than 2 meq./100 g. of soil. Yields increased with increasing soil pH, but the presence of free salts in this heavily fertilized soil made pH an unreliable criterion for determining the need for liming. Applying 8 tons of limestone per acre to the surface of a very acid Cialitos clay before planting increased cane yields from an average of 12.4 to 34.5 tons per acre, and decreased exchangeable Al from 7.3 to 0.5 meq. per 100 g. of soil. The foliar composition at 9 months of age, and the sucrose content of the sugarcane were not affected by the soil factors studied, or by lime applications, and remained unchanged, at satisfactory levels, in plots yielding from almost 0 to over 40 tons of cane per acre. A survey showed that in many sugarcane soils of the Humid Region exchangeable aluminum exceeded levels that depressed cane yields on Cialitos clay in this experiment.

scholarly journals Extent, Distribution, and Causes of Soil Acidity under Subsistence Farming System and Lime Recommendation: The Case in Wolaita, Southern Ethiopia

2021 ◽  
Vol 2021 ◽  
pp. 1-9
Author(s):  
Fanuel Laekemariam ◽  
Kibebew Kibret
Keyword(s):  
Soil Fertility ◽  
Soil Ph ◽  
Soil Acidification ◽  
Soil Acidity ◽  
Farmyard Manure ◽  
Southern Ethiopia ◽  
Subsistence Farming ◽  
Exchangeable Acidity ◽  
Management Interventions ◽  
Exchangeable Al

Soil acidity is one of the most important environmental threats to the Ethiopian highlands where the livelihood of the majority of people is reliant on agriculture. Yet, information regarding its extent, distribution, causes, and lime requirement at a scale relevant to subsistence farming systems is still lacking. This study (1) investigates the extent and spatial distribution of soil acidity, (2) identifies factors attributing to soil acidification, and (3) predicts the lime requirement for major crops. A total of 789 soil samples were collected from arable lands in the Wolaita area which is mainly characterized by poor soil fertility and soil degradation in southern Ethiopia. Results revealed that the landscape is characterized by a gentle slope followed by strongly sloppy > flat > hilly topographies. Clay is the dominant soil textural class. A soil pH map, which is generated using geospatial analysis, demonstrates that 3.3, 78.0, and 18.7% of the total area were under strongly acidic, moderately acidic, and neutral soil reactions, respectively. The exchangeable acidity (Cmol(+)/kg) varied from nil to 5.1, whereas exchangeable Al ranged from 1.4 to 19.9 Cmol(+)/kg. The soil pH has shown a significantly ( p  < 0.001) negative association with clay content (r = −0.33), exchangeable Al (r = −61), exchangeable acidity (r = −0.58), and inorganic fertilizer application (r = −0.33). Increased rates of diammonium phosphate (DAP) (r2 = 0.91) and urea (r2 = 0.88) markedly elevated soil acidity. Conversely, manuring showed a significant ( p  < 0.001) and positive relationship with pH (r = 0.37) in which the increasing rate of manure significantly reduced acidification (r2 = 0.98). DAP and urea applications above 75 kg/ha lowered soil pH units by 0.56 and 0.48, respectively, <25 kg/ha while at the same time farmyard manure (FYM) at 4 t/ha raised pH by 0.75 units over the unfertilized field. Residue management significantly ( p  < 0.001) influenced soil pH wherein it ranged from 6.09 (complete residue removal) to 6.61 (residue incorporation). Changes in land use, cropping intensity, and socioeconomic status were also significantly attributed to soil acidification. To curb the effects of soil acidity, the lime requirement for common bean growing fields varied from zero to 6.6 t/ha, while for maize it was between zero and 4.3 t/ha. It is concluded that soil management interventions such as maintaining and incorporating crop residues, integrated use of organic and inorganic fertilizers, liming, and enhancing farmers’ awareness should be advocated to overcome soil acidification and improve soil fertility. In addition, introducing crops with traits that tolerate acidity and Al toxicity is also suggested.

The inhibition effect of tea polyphenols on soil nitrification is greater than denitrification in tea garden soil

2021 ◽  
Vol 778 ◽  
pp. 146328
Author(s):  
Sheng Tang ◽  
Qingxu Ma ◽  
Jipeng Luo ◽  
Yinan Xie ◽  
Muhammad Laeeq ur Rehman Hashmi ◽  
...  
Keyword(s):  
Tea Polyphenols ◽  
Garden Soil ◽  
Soil Nitrification ◽  
Inhibition Effect ◽  
Tea Garden

scholarly journals Fractionation and Bioavailability of Trace Elements in Wuyi Rock Tea Garden Soil

2018 ◽  
Vol 27 (1) ◽  
pp. 421-430 ◽  
Author(s):  
Hongmeng Ye ◽  
Guoping Li ◽  
Xuyin Yuan ◽  
Maozhong Zheng
Keyword(s):  
Trace Elements ◽  
Garden Soil ◽  
Tea Garden

scholarly journals IMMOBILIZATION OF EXCHANGEABLE CROMIUM IN A CONTAMINATED SOIL USING NATURAL ZEOLITE AS AN EFFECTIVE ADSORBENT

2020 ◽  
Vol 58 (5A) ◽  
pp. 10
Author(s):  
Van Minh Dang ◽  
Huu Tap Van ◽  
Thi Bich Hanh Nguyen ◽  
Dinh Vinh Nguyen ◽  
Thị Tuyet Nguyen ◽  
...  
Keyword(s):  
Soil Ph ◽  
Contaminated Soil ◽  
Contaminated Soils ◽  
Natural Zeolite ◽  
Organic Matters ◽  
Amended Soils ◽  
Mn Oxide ◽  
Content Ratio ◽  
Incubation Experiments ◽  
Exchangeable Fraction

This work investigated the effects of soil pH and the content ratio of natural zeolite on Cr contaminated soil. The immobilization experiments of the exchangeable Cr in contaminated soils were conducted using the batch method. The incubation experiments were carried out over 30 days in plastic bottles to determine five fraction of Cr existence (exchangeable fraction (F1), Fe/Mn/Oxide (F2), carbonate bound (F3), organic matters (F4) and residual (F5)) in amended soils after incubation. Results showed that the content and proportion of the exchangeable Cr decreased with an increase in soil pH from 5 to 9. At soil pH 5, the exchangeable Cr in soil reduced from 44.80±0.772 mg/kg (initial soil) to 17.72±0.300 mg/kg after 30 days of incubation with natural Zeolite 3%. Meanwhile, the exchangeable Cr of soil also decreased with increasing the content ratio of natural zeolite from 1% to 5% in soil. The ratio of 3% was suitable for incubation of the exchangeable Cr in contaminated soil with natural zeolite. The exchangeable Cr in contaminated soil decreased from 80.34% at un-amended soil treatment to 25.06% after incubation of 30 days. The forms of carbonate bound (F3) and organic matters (F4) in amended soils increased to 36.54% and 28% compared with 4.26% and 6.90% in un-amended contaminated soil. Ion exchange, precipitation and adsorption on the surface of natural zeolite  might be the potential mechanisms of immobilization of the exchangeable Cr. The results indicated that natural zeolite can be used as the effective adsorbent for immobilizing the exchangeable Cr in contaminated soils and leading to a decrease in the environmental risk from Cr toxicity.

scholarly journals Changes in Soil Phosphorus Pools and Chemical Properties under Liming in Nitisols of Farawocha, South Ethiopia

2021 ◽  
Vol 2021 ◽  
pp. 1-11
Author(s):  
Fikeremareyam Chulo ◽  
Fanuel Laekemariam ◽  
Alemayehu Kiflu
Keyword(s):  
Soil Ph ◽  
Nutrient Dynamics ◽  
Soil Phosphorus ◽  
Acid Soil ◽  
Chemical Properties ◽  
Soil Chemical Properties ◽  
Southern Ethiopia ◽  
Organic Part ◽  
Exchangeable Acidity ◽  
P Pools

Understanding the nutrient dynamics in acid soil is fundamental to carry out proper management. The study was conducted to investigate phosphorus (P) pools and selected properties under different rates of lime for acid nitisols of Farawocha, Southern Ethiopia. Four lime rates incubated for a month in three replications were tested. The lime rates were 0 t/ha (0%), 5.25 t/ha (50%), 10.5 t/ha (100%), and 15.75 t/ha (150%). Lime requirement (LR) for 100% was calculated targeting soil pH of 6.5. Data on the P pools such as soluble P (P-sol) and bounded forms of P with iron (Fe-P), aluminum (Al-P), calcium (Ca-P), organic part (Org-P), residual P (Res-P), and total of P fractions were measured. In addition, changes in soil chemical properties such as pH, exchangeable acidity, calcium (Ca), magnesium (Mg), sulfur (S), iron (Fe), copper (Cu), boron (B), zinc (Zn), and manganese (Mn) were analyzed. The result showed that total P was 357.5 mg/kg. Compared to nontreated soil, liming at a rate of 15.75 t/ha significantly improved P-sol (34.2%, r2 = 0.88), Ca-P (61.6%, r2 = 0.92), and Res-P (195%, r2 = 0.94); however, it reduced Fe-P (58.5%, r2 = −0.83), Al-P (71%, r2 = −0.97), and Org-P (19.1%, r2 = 0.93). Overall, the P-associated fractions in the soil, regardless of the lime rates, were in the order of Org_P > Res_P > Fe_P > Ca_P > Al_P > P-sol. Liming raised soil pH by 2.1 units (4.5 to 6.6) over nonlimed soil, whereas it reduced exchangeable acidity from 4.18 to 0.23 meq/100 g soil. Available P, Ca, Mg, S, Cu, Zn, and B contents were significantly improved with lime application. However, liming reduced Fe and Mn contents. In conclusion, these findings showed that liming facilitated the release of P from various pools, modified pH and exchangeable acidity, and resulted in beneficial changes for most of the soil chemical properties.

scholarly journals Crop Response to Soil Acidity Factors in Ultisols and Oxisols in Puerto Rico. XII. Tomatoes

1969 ◽  
Vol 69 (3) ◽  
pp. 357-365
Author(s):  
Edmundo Rivera ◽  
José Rodríguez ◽  
Fernando Abruña
Keyword(s):  
Puerto Rico ◽  
Cation Exchange ◽  
Soil Ph ◽  
Cation Exchange Capacity ◽  
Soil Acidity ◽  
Exchange Capacity ◽  
Crop Response ◽  
Exchangeable Al

The effect of acidity factors of two Ultisols and one Oxisol on yield and foliar composition of tomatoes was determined. Yields were not markedly reduced by acidity in the Ultisols until pH dropped to around 4.6 with 45% Al saturation of the cation exchange capacity (CEC), and no yield was produced at about pH 4.1 and 80% Al saturation. In the Oxisol, tomato yields dropped steadily from 39.7 t/ha, when there was no exchangeable AI, to 17.5 t/ha at the highest level of acidity, pH 4.4 and 43% AI saturation. In all soils, yields were closely correlated with soil pH, exchangeable Al and Ca and Al/Ca.

Effects of biochars generated from crop residues on chemical properties of acid soils from tropical and subtropical China

Soil Research ◽  
2012 ◽  
Vol 50 (7) ◽  
pp. 570 ◽  
Author(s):  
Jin-Hua Yuan ◽  
Ren-Kou Xu
Keyword(s):  
Soil Ph ◽  
Crop Residues ◽  
Chemical Properties ◽  
Acid Soils ◽  
Base Cations ◽  
Exchange Capacity ◽  
Chemical Compositions ◽  
Subtropical China ◽  
Exchangeable Base Cations ◽  
Exchangeable Acidity

The chemical compositions of biochars from ten crop residues generated at 350°C and their effects on chemical properties of acid soils from tropical and subtropical China were investigated. There was greater alkalinity and contents of base cations in the biochars from legume residues than from non-legume residues. Carbonates and organic anions of carboxyl and phenolic groups were the main forms of alkalis in the biochars, and their relative contributions to biochar alkalinity varied with crop residues. Incubation experiments indicated that biochar incorporation increased soil pH and soil exchangeable base cations and decreased soil exchangeable acidity. There were greater increases in soil pH and soil exchangeable base cations, and a greater decrease in soil exchangeable acidity, for biochars from legume than from non-legume residues. The biochars did not increase the cation exchange capacity (CEC) of soils with relatively high initial CEC but did increase the CEC of soils with relatively low initial CEC at an addition level of 1%. The incorporation of biochars from crop residues not only corrected soil acidity but also increased contents of potassium, magnesium, and calcium in these acid soils from tropical and subtropical regions and thus improved soil fertility.

Effect of Trifluralin and Metribuzin Combinations on Soybean Tolerance to Metribuzin

Weed Science ◽  
1977 ◽  
Vol 25 (1) ◽  
pp. 88-93 ◽  
Author(s):  
James S. Ladlie ◽  
William F. Meggitt ◽  
Donald Penner
Keyword(s):  
Glycine Max ◽  
Soil Ph ◽  
Root Development ◽  
Field Trials ◽  
Soybean Plant ◽  
Ph Values ◽  
High Soil

In field trials, soybeans [Glycine max(L.) Merr.] treated with trifluralin [α,α,α-trifluoro-2,6-dinitro-N,N-dipropyl-p-toluidine] at 0.56 and 0.84 kg/ha were protected from injury by metribuzin [4-amino-6-tert-butyl-3-(methylthio-as-triazine-5(4H)one] at 0.28 to 1.12 kg/ha. Soybean injury from metribuzin at high soil pH values was reduced by applying it in combination with trifluralin. Trifluralin also protected soybeans from injury caused by low rates of atrazine [2-chloro-4-(ethylamino)-6-(isopropylamino)-s-triazine] greenhouse studies. The trifluralin treatment reduced root development and greatly reduced14C-atrazine and14C-metribuzin uptake and content within the soybean plant.

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