scholarly journals Effect on Chemical and Physical Properties of Soil Each Peat Moss, Elemental Sulfur, and Sulfur-Oxidizing Bacteria

Plants ◽  
2021 ◽  
Vol 10 (9) ◽  
pp. 1901
Author(s):  
So-Young Lee ◽  
Eun-Gyeong Kim ◽  
Jae-Ryoung Park ◽  
Young-Hyun Ryu ◽  
Won Moon ◽  
...  
Keyword(s):  
Soil Ph ◽  
Elemental Sulfur ◽  
Organic Matter Content ◽  
Matter Content ◽  
Peat Moss ◽  
Soil Environment ◽  
Biological Factors ◽  
Sulfur Oxidizing ◽  
Properties Of Soil ◽  
Sulfur Oxidizing Bacteria

Peat moss is an organic substance corroded by sphagnum moss and has a pH of 3.0–4.0. Elemental sulfur is sulfated and oxidized by the action of bacteria to become sulfuric acid. These biological factors can alter the soil environment. Blueberries require soil with a pH of 4.5–5.2 and high organic matter content. In this experiment, we investigated whether different treatment rates of peat moss, elemental sulfur, and sulfur-oxidizing bacteria affect changes in soil pH, physicochemical properties, and electrical conductivity. We detected strong changes in soil pH as a reaction to the supply of peat moss, elemental sulfur, and sulfur-oxidizing bacteria. The pH of the soil when peat moss and elemental sulfur each were supplied was reduced. In addition, the pH decreased faster when elemental sulfur and sulfur-oxidizing bacteria were supplied together than elemental sulfur alone, satisfying an acidic soil environment suitable for blueberry cultivation. In this experiment, it is shown that peat moss, elemental sulfur, and sulfur-oxidizing bacteria are suitable for lowering soil pH. It was demonstrated that when elemental sulfur and sulfur-oxidizing bacteria were treated together, the pH decreased faster than when treated with peat moss. It could be economically beneficial to farmers to use elemental sulfur and sulfur-oxidizing bacteria, which are cheaper than peat moss, to reduce the pH of the soil.

scholarly journals BIODEGRADATION OF CATTLE HORN SHAVINGS IN SOIL AND ITS EFFECT ON THE AGROCHEMICAL PROPERTIES OF SOIL / GALVIJŲ RAGŲ DROŽLIŲ BIODEGRADACIJA DIRVOŽEMYJE IR JOS ĮTAKA AGROCHEMINĖMS DIRVOŽEMIO SAVYBĖMS

2014 ◽  
Vol 6 (4) ◽  
pp. 368-372
Author(s):  
Edita Mažuolytė-Miškinė ◽  
Ilona Grigalavičienė ◽  
Violeta Gražulevičienė
Keyword(s):  
Organic Matter ◽  
Soil Ph ◽  
Organic Matter Content ◽  
Matter Content ◽  
Organic Production ◽  
Specific Electrical Conductivity ◽  
Laboratory Conditions ◽  
Agrochemical Properties ◽  
Field And Laboratory Conditions ◽  
Properties Of Soil

The article presents investigation into the rate of the biodegradation of cattle horn shavings used as plant fertilisers in soil and describes their effect on the agrochemical properties of soil. Research was carried out under field and laboratory conditions. The field experiment was conducted on the farm of organic production at the Centre of Agroecology of Aleksandras Stulginskis University, Lithuania in May – August of 2012. The average air temperature during the experiment was 16.45 °C. Soil pH, specific electrical conductivity value and organic matter content in soil samples were measured. The extent of the biodegradation of cattle horn shavings in soil and in the thermostat under laboratory conditions at the temperatures of 5 °C and 20 °C and at 40% soil moisture was compared. The obtained results indicate that mass changes in cattle horn shavings in the process of biodegradation under field and laboratory conditions (at an ambient temperature of 5 °C and 20 °C) are similar: after 120 days, the mass of horn shavings decreased by 37.3%, 36.2%, and 34.5% respectively. The largest changes in soil pH and organic matter content were observed during the first 60 days. During the biodegradation of horn shavings under field conditions after 40 days, organic matter content in soil increased from 2.53 to 3.20% and soil pH decreased from 8.0 to 7.1. Smaller changes were observed under laboratory conditions. Ištirta augalams tręšti naudojamų galvijų ragų drožlių suirimo sparta dirvožemyje ir jų įtaka dirvožemio savybėms. Bandymai atlikti lauko (natūraliomis gamtinėmis) ir laboratorinėmis sąlygomis. Lauko eksperimentas vykdytas 2012 m. gegužės–rugpjūčio mėnesiais Aleksandro Stulginskio universiteto Agroekologijos centro ekologinės gamybos ūkyje. Vidutinė oro temperatūra bandymų laikotarpiu buvo 16,45 °C. Laboratorinio eksperimento metu buvo nustatomas ragų drožlių suirimo greitis dirvožemyje esant 5 ir 20 °C aplinkos temperatūrai ir 40 % dirvožemio drėgniui. Atlikti dirvožemio pH, savitojo elektrinio laidžio ir organinės medžiagos kiekio dirvožemyje tyrimai. Nustatyta, kad ragų drožlių masės pokyčiai biodegraduojant drožlėms lauko sąlygomis ir laboratorinėmis sąlygomis, esant 5 ir 20 °C aplinkos temperatūrai, yra panašūs: ragų drožlių masė po 120 parų sumažėjo atitinkamai 37,3 %, 36,2 %, ir 34,5 %. Didžiausi dirvožemio pH ir organinės medžiagos kiekio pokyčiai vyko per pirmąsias 60 parų. Ragų drožlėms biodegraduojant lauko sąlygomis organinės medžiagos kiekis dirvožemyje šiuo laikotarpiu padidėjo nuo 2,53 ik 3,20 %, o dirvožemio pH sumažėjo nuo 8,0 iki 7,1. Atliekant bandymus laboratorinėmis sąlygomis šie pokyčiai buvo mažesni.

scholarly journals Effect of Clay, Soil Organic Matter, and Soil pH on Initial and Residual Weed Control with Flumioxazin

Agronomy ◽  
2021 ◽  
Vol 11 (7) ◽  
pp. 1326
Author(s):  
Calvin F. Glaspie ◽  
Eric A. L. Jones ◽  
Donald Penner ◽  
John A. Pawlak ◽  
Wesley J. Everman
Keyword(s):  
Organic Matter ◽  
Soil Organic Matter ◽  
Weed Control ◽  
Soil Ph ◽  
Organic Matter Content ◽  
Amaranthus Retroflexus ◽  
Matter Content ◽  
Weed Species ◽  
Soil Organic Matter Content ◽  
Field Soils

Greenhouse studies were conducted to evaluate the effects of soil organic matter content and soil pH on initial and residual weed control with flumioxazin by planting selected weed species in various lab-made and field soils. Initial control was determined by planting weed seeds into various lab-made and field soils treated with flumioxazin (71 g ha−1). Seeds of Echinochloa crus-galli (barnyard grass), Setaria faberi (giant foxtail), Amaranthus retroflexus (redroot pigweed), and Abutilon theophrasti (velvetleaf) were incorporated into the top 1.3 cm of each soil at a density of 100 seeds per pot, respectively. Emerged plants were counted and removed in both treated and non-treated pots two weeks after planting and each following week for six weeks. Flumioxazin control was evaluated by calculating percent emergence of weeds in treated soils compared to the emergence of weeds in non-treated soils. Clay content was not found to affect initial flumioxazin control of any tested weed species. Control of A. theophrasti, E. crus-galli, and S. faberi was reduced as soil organic matter content increased. The control of A. retroflexus was not affected by organic matter. Soil pH below 6 reduced flumioxazin control of A. theophrasti, and S. faberi but did not affect the control of A. retroflexus and E. crus-galli. Flumioxazin residual control was determined by planting selected weed species in various lab-made and field soils 0, 2, 4, 6, and 8 weeks after treatment. Eight weeks after treatment, flumioxazin gave 0% control of A. theophrasti and S. faberi in all soils tested. Control of A. retroflexus and Chenopodium album (common lambsquarters) was 100% for the duration of the experiment, except when soil organic matter content was greater than 3% or the soil pH 7. Eight weeks after treatment, 0% control was only observed for common A. retroflexus and C. album in organic soil (soil organic matter > 80%) or when soil pH was above 7. Control of A. theophrasti and S. faberi decreased as soil organic matter content and soil pH increased. Similar results were observed when comparing lab-made soils to field soils; however, differences in control were observed between lab-made organic matter soils and field organic matter soils. Results indicate that flumioxazin can provide control ranging from 75–100% for two to six weeks on common weed species.

scholarly journals Nitrogen mineralization and microbial activity as influenced by sulfur sources in an alkaline calcareous soil

1970 ◽  
pp. 14-18
Author(s):  
Tufail Shah ◽  
Zahir Shah ◽  
Syed Atizaz Ali Shah ◽  
Nazir Ahmad
Keyword(s):  
Organic Matter ◽  
Sulfuric Acid ◽  
Microbial Activity ◽  
Calcareous Soil ◽  
Bacterial Population ◽  
Elemental Sulfur ◽  
Microbial Population ◽  
Organic Matter Content ◽  
Matter Content ◽  
Fungal Population

A study was performed to check the effects of various sources of sulfur on microbial activity, microbial population, N mineralization and organic matter content in an alkaline calcareous soil by using soil samples collected from Malakandher Farm at 0-20 cm depth, and analyzed for microbial activity, total mineral nitrogen, bacterial and fungal population and organic matter content. The results showed that the rate of CO2 evolution and cumulative CO2 production were higher in soils amended with elemental sulfur followed by sulfuric acid and gypsum treated soils. The microbial activity decreased with incubation period in all treatments, and the microbial population was greatly affected by sulfur sources. Generally, the bacterial population decreased in soils amended with elemental sulfur, but the population was higher in soils amended with gypsum. Bacterial population was suppressed in soils treated with sulfuric acid. However, the fungal population was higher in soils amended with sulfuric acids was less in soil amended with elemental sulfur. The sulfur amendments promoted immobilization of N. The net N immobilized was higher in soil amended with gypsum followed by soils amended with sulfuric acid and elemental sulfur. The percent organic matter was higher in soils amended with gypsum and was decreased compared with that amended with elemental sulfur or sulfuric acid. These results suggested that soil microbiological properties changed with sulfur amendments during laboratory incubation.

scholarly journals Organic Stabilization of Extracellular Elemental Sulfur in a Sulfurovum-Rich Biofilm: A New Role for Extracellular Polymeric Substances?

2021 ◽  
Vol 12 ◽  
Author(s):  
Brandi Cron ◽  
Jennifer L. Macalady ◽  
Julie Cosmidis
Keyword(s):  
Crystal Structures ◽  
Extracellular Polymeric Substances ◽  
Elemental Sulfur ◽  
Dense Matrix ◽  
Cave System ◽  
Carboxylic Groups ◽  
Sulfur Oxidizing ◽  
New Evidence ◽  
Sulfur Oxidizing Bacteria

This work shines light on the role of extracellular polymeric substance (EPS) in the formation and preservation of elemental sulfur biominerals produced by sulfur-oxidizing bacteria. We characterized elemental sulfur particles produced within a Sulfurovum-rich biofilm in the Frasassi Cave System (Italy). The particles adopt spherical and bipyramidal morphologies, and display both stable (α-S8) and metastable (β-S8) crystal structures. Elemental sulfur is embedded within a dense matrix of EPS, and the particles are surrounded by organic envelopes rich in amide and carboxylic groups. Organic encapsulation and the presence of metastable crystal structures are consistent with elemental sulfur organomineralization, i.e., the formation and stabilization of elemental sulfur in the presence of organics, a mechanism that has previously been observed in laboratory studies. This research provides new evidence for the important role of microbial EPS in mineral formation in the environment. We hypothesize that the extracellular organics are used by sulfur-oxidizing bacteria for the stabilization of elemental sulfur minerals outside of the cell wall as a store of chemical energy. The stabilization of energy sources (in the form of a solid electron acceptor) in biofilms is a potential new role for microbial EPS that requires further investigation.

Lime loss rates from arable and grassland soils

1998 ◽  
Vol 131 (4) ◽  
pp. 455-464 ◽  
Author(s):  
B. J. CHAMBERS ◽  
T. W. D. GARWOOD
Keyword(s):  
Organic Matter ◽  
Soil Ph ◽  
Agricultural Land ◽  
Negative Relationship ◽  
Organic Matter Content ◽  
Matter Content ◽  
N Fertilizer ◽  
Exchangeable Ca ◽  
Water Ph ◽  
Loss Rates

Lime loss rates were determined for 11 agricultural soils across England (1987–92) under arable cropping (six sites) and grassland management (five sites), receiving commercial rates of fertilizer inputs. Lime additions in the range 0–1500 kg ha−1 CaCO3 (250 kg ha−1 CaCO3 increments) were made annually to the sites. Soil pH (water and 0·01 m CaCl2) and exchangeable calcium concentrations were measured annually. The annual lime loss rates were calculated as the amount of lime needed to maintain the initial site pH or exchangeable Ca concentrations.Lime loss rates based on soil water pH varied between 40 and 1270 kg ha−1 CaCO3, on the basis of CaCl2 pH between 0 and 1370 kg ha−1 CaCO3, and exchangeable Ca between 0 and 1540 kg ha−1 CaCO3. There was a positive relationship between the lime loss rate (based on water pH) and initial soil pH value (r=0·75; P<0·01), and a negative relationship with soil organic matter content (r=0·63; P<0·05) was based on soil pH, organic matter content and nitrogen (N) fertilizer input. Lime loss rates were approximately double those predicted by previous models developed in the 1970s, reflecting the greater quantities of inorganic N fertilizer now being applied to agricultural land.

scholarly journals Innovative Methods for Soil DNA Purification Tested in Soils with Widely Differing Characteristics

2008 ◽  
Vol 74 (9) ◽  
pp. 2902-2907 ◽  
Author(s):  
Marketa Sagova-Mareckova ◽  
Ladislav Cermak ◽  
Jitka Novotna ◽  
Kamila Plhackova ◽  
Jana Forstova ◽  
...  
Keyword(s):  
Dna Extraction ◽  
Soil Ph ◽  
Vegetation Cover ◽  
Organic Matter Content ◽  
Clay Content ◽  
Matter Content ◽  
Soil Dna ◽  
Innovative Methods ◽  
Soil Dna Extraction ◽  
Extraction And Purification

ABSTRACT Seven methods of soil DNA extraction and purification were tested in a set of 14 soils differing in bedrock, texture, pH, salinity, moisture, organic matter content, and vegetation cover. The methods introduced in this study included pretreatment of soil with CaCO3 or purification of extracted DNA by CaCl2. The performance of innovated methods was compared to that of the commercial kit Mo Bio PowerSoil and the phenol-chloroform-based method of D. N. Miller, J. E. Bryant, E. L. Madsen, and W. C. Ghiorse (Appl. Environ. Microbiol. 65:4715-4724, 1999). This study demonstrated significant differences between the tested methods in terms of DNA yield, PCR performance, and recovered bacterial diversity. The differences in DNA yields were correlated to vegetation cover, soil pH, and clay content. The differences in PCR performances were correlated to vegetation cover and soil pH. The innovative methods improved PCR performance in our set of soils, in particular for forest acidic soils. PCR was successful in 95% of cases by the method using CaCl2 purification and in 93% of cases by the method based on CaCO3 pretreatment, but only in 79% by Mo Bio PowerSoil, for our range of soils. Also, the innovative methods recovered a higher percentage of actinomycete diversity from a subset of three soils. Recommendations include the assessment of soil characteristics prior to selecting the optimal protocol for soil DNA extraction and purification.

scholarly journals Studies on some zoosporic fungi in soils of Upper Egypt

2014 ◽  
Vol 27 (1) ◽  
pp. 159-170 ◽  
Author(s):  
S. K. Hassan ◽  
E. M. Fadl-Allah
Keyword(s):  
Organic Matter Content ◽  
Chemical Properties ◽  
Calcium Content ◽  
Matter Content ◽  
Physical And Chemical Properties ◽  
Soluble Salts ◽  
Unidentified Species ◽  
Physical And Chemical ◽  
Properties Of Soil ◽  
And Chemical Properties

In the present paper forty-five zoosporic members of the aquatic fungi as well as some unidentified species belonging to seventeen genera were recorded <i>Nowakowskiella, Saprolegnia, Pythium, Rhizohlyctis</i> and <i>Achlya</i> were the most common genera of occurrence. Some physical and chemical properties of soil such as temperature calcium content total soluble salts and organic matter content are positively correlated with the of population zoosporic fungal.

scholarly journals Accumulation of diazinon in Indian spinach under different doses of rice hull

2017 ◽  
Vol 26 (2) ◽  
pp. 125-131
Author(s):  
Fahmida Akhter ◽  
Didar Ul Alam ◽  
Monira Begum ◽  
Naushad Alam
Keyword(s):  
Organic Matter ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Matter Content ◽  
Rice Hull ◽  
Vegetable Crops ◽  
Soil Organic Matter Content ◽  
Positive Effect ◽  
Different Doses ◽  
Properties Of Soil

An experiment was conducted to determine the effect of diazinon pesticide on some chemical properties of soil and to evaluate the accumulation of diazinon in Indian spinach (Basilla alba) under different doses of rice hull. Diazinon application had a positive effect to reduce the electrical conductivity (EC) of soil. Values of pH were found to decrease with the addition of diazinon. Diazinon had no effect on soil organic matter content although addition of rice hull increased organic matter content in soil with time. Plant analysis showed that the application of rice hull restricted the uptake of diazinon and continuously decreased with time. Therefore, rice hull could be used to control the uptake of diazinon pesticide by short duration vegetable crops. Dhaka Univ. J. Biol. Sci. 26(2): 125-131, 2017 (July)

scholarly journals Chemical and Physical Properties of Soil Amended with Pecan Wood Chips

HortScience ◽  
2008 ◽  
Vol 43 (3) ◽  
pp. 891-896 ◽  
Author(s):  
Mohammed B. Tahboub ◽  
William C. Lindemann ◽  
Leigh Murray
Keyword(s):  
Physical Properties ◽  
Soil Ph ◽  
Organic Matter Content ◽  
Wood Chip ◽  
Aggregate Stability ◽  
Application Rate ◽  
Matter Content ◽  
Wood Chips ◽  
Silty Clay ◽  
Application Rates

The pruning wood of pecan [Carya illinoinensis (Wangenh.) K. Koch] is often burned. Chipping and soil incorporation of pruning wood is becoming more popular as a result of environmental constraints on burning. The objective of our research was to determine how pecan wood incorporation into soil affects the soil chemical and physical properties. Pecan wood chips were incorporated into a silty clay soil at rates of 0, 4484, 8968, 13,452, and 17,936 kg·ha−1 in Summer 2002, 2003, and 2004. Some plots received nitrogen at a rate of 0, 15.2, 30.5, 45.7, and 61.0 kg·ha−1 to adjust the C : N ratio of trimmings to 30 : 1. Ammonium sulfate, as a nitrogen source to balance the C : N ratio of pecan wood chips, reduced soil pH. However, the wood chip amendments alone did not reduce soil pH. Soil salinity (as determined by electrical conductivity) and bulk density were unaffected by wood chip incorporation regardless of application rate or number of applications. Incorporation of pecan chips had little effect on soil moisture content, but the soil had an inherently high waterholding capacity. Pecan wood chip incorporation significantly increased soil organic matter content and aggregate stability, particularly at the higher application rates and with repeated amendment. The incorporation of pecan pruning wood into the soil appears to improve soil tilth and aggregation while providing growers with an environmentally acceptable means of disposal.

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