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.

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 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 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.

Effect of Tillage and Cover Crop on Fluometuron Adsorption and Degradation under Controlled Conditions

Weed Science ◽  
1994 ◽  
Vol 42 (4) ◽  
pp. 629-634 ◽  
Author(s):  
Blake A. Brown ◽  
Robert M. Hayes ◽  
Donald D. Tyler ◽  
Thomas C. Mueller
Keyword(s):  
Organic Matter ◽  
Soil Organic Matter ◽  
Soil Ph ◽  
Cover Crop ◽  
Soil Depth ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Matter Content ◽  
No Till

Fluometuron adsorption and degradation were determined in soil collected at three depths from no-till + no cover, conventional-till + no cover, no-till + vetch cover, and conventional-till + vetch cover in continuous cotton. These combinations of tillage + cover crop + soil depth imparted a range of organic matter and pH to the soil. Soil organic matter and pH ranged from 0.9 to 2.5% and from 4.7 to 6.5, respectively. Fluometuron adsorption was affected by soil depth, tillage, and cover crop. In surface soils (0 to 4 cm), fluometuron adsorption was greater in no-till + vetch plots than in conventional-tilled + no cover plots. Soil adsorption of fluometuron was positively correlated with organic matter content and cation exchange capacity. Fluometuron degradation was not affected by adsorption, and degradation empirically fit a first-order model. Soil organic matter content had no apparent effect on fluometuron degradation rate. Fluometuron degradation was more rapid at soil pH > 6 than at pH ≤ 5, indicating a potential shift in microbial activity or population due to lower soil pH. Fluometuron half-life ranged from 49 to 90 d. These data indicate that tillage and cover crop may affect soil dissipation of fluometuron by altering soil physical and chemical properties that affect fluometuron degrading microorganisms or bioavailability.

scholarly journals Comparative Chemical Characterisation of Soils at Cypripedium Calceolus Sites in Latvia

2017 ◽  
Vol 71 (1-2) ◽  
pp. 43-51
Author(s):  
Dace Kļaviņa ◽  
Anita Osvalde
Keyword(s):  
Organic Matter ◽  
Soil Ph ◽  
Nutrient Concentration ◽  
Species Abundance ◽  
Organic Matter Content ◽  
Matter Content ◽  
Organic Soils ◽  
Strong Impact ◽  
Related Factors ◽  
Cypripedium Calceolus

Abstract The main aim of the study was to evaluate the soil chemical characteristics of Cypripedium calceolus sites in Latvia for understanding of the species ecology, and its conservation problems and possibilities. Soil for 27 C. calceolus sites in Latvia was analysed during 2007-2015. The concentration of plant available essential nutrients (N, P, K, Ca, Mg, S, Fe, Mn, Zn, Cu, Mo, B), soil pH, electrical conductivity and concentration of organic matter were determined. Nutrient concentration of C. calceolus leaf samples from six sites were determined. The results demonstrated high heterogeneity in soil chemical composition with high variation for Ca, Mg, and Mn. The results suggest some relationship between soil organic matter content and size of the orchid population. Soil pH and Ca concentration did not affect the size and vitality of C. calceolus populations in Latvia. There was no significant correlation between nutrient concentration in soil and C. calceolus leaves suggesting strong impact of other soil-related factors in determining the availability of nutrients. In general, the levels of N, P, K, Ca, Mg, Fe, Mn, and Zn concentrations in C. calceolus leaves were adequate or slightly decreased for successful orchid growth. The study showed deficiency of S, Cu, and B in the vast majority of leaf samples. C. calceolus sites in Latvia occur mainly on organic soils or mineral soils with high content of organic matter. There was a weak positive correlation (r = 0.21) observed only between total number of ramets of C. calceolus in site and Ca concentration in the soil, suggesting that soil properties are not a main factor affecting species abundance in the site.

scholarly journals Influence of different stands of sal (Shorea robusta C. F. Gaertn.) forest of Bangladesh on soil health

2015 ◽  
Vol 2 (1) ◽  
pp. 17-25
Author(s):  
Mohammad Kamrul Hasan ◽  
Md Bayeazid Mamun
Keyword(s):  
Electrical Conductivity ◽  
Organic Matter ◽  
Soil Ph ◽  
Soil Health ◽  
Organic Matter Content ◽  
Matter Content ◽  
Mixed Stand ◽  
Pure Stand ◽  
Total N ◽  
Exchangeable K

The study was conducted in Dukhula sadar and Gasabari forest range under Madhupur Sal Forest of Bangladesh to determine the soil nutrient composition and isolation of fungi with varying stands. Three stands viz. pure sal, plantation and mixed were considered as treatment of the study. A quadrate sample plot of 10×10 m2 size was measured to collect soil samples for both chemical analysis and fungi isolation. Soil pH, electrical conductivity, organic matter content, total N, available P, exchangeable K, available S, fungal abundance and colony character (cm) were determined to achieve the objective of the study. The results revealed that soil pH and electrical conductivity were highest (6.61 and 21.10?S/cm) in mixed stand and lowest (6.38 and 10.75?S/cm) in pure stand. Organic matter content and total N were highest (2.24 and 0.145%) in plantation stand and lowest (1.65 and 0.112%) in mixed and pure stand, respectively. Available P, exchangeable K and available S were highest (3.65, 98.66 and 17.53ppm) in pure stand and lowest (1.97, 79.49 and 10.25ppm) in plantation stand. In addition, four fungal genera Sclerotium, Rhizoctonia, Pythium and Verticillium were identified in the study area soils. The highest fungal population (entire genus except Verticillium) (colony number/g soil) was found in mixed stand while it was found lowest in pure (Sclerotium ) and plantation stand (Rhizoctonia and Pythium ). There was no significant variation in colony diameter of the fungi among the treatments. Therefore, it can be concluded that better soil health was maintained in natural forest rather than plantation forest.Res. Agric., Livest. Fish.2(1): 17-25, April 2015

scholarly journals Soil pH and Nutrient Characteristics of Newly-added Cultivated Land in Heyang, China

2020 ◽  
Vol 204 ◽  
pp. 01013
Author(s):  
Gang Li ◽  
Ruiqing Zhang ◽  
Ying Wang ◽  
Nan Lu ◽  
Yang Wei ◽  
...  
Keyword(s):  
Organic Matter ◽  
Soil Organic Matter ◽  
Total Nitrogen ◽  
Soil Ph ◽  
Ph Value ◽  
Organic Matter Content ◽  
Matter Content ◽  
Available Phosphorus ◽  
Cultivated Land ◽  
Soil Available Phosphorus

In order to understand the soil pH and main nutrient characteristics of newly added cultivated land in the eastern part of Guanzhong, and 160 soil samples were collected in 2016, the soil pH, organic matter, total nitrogen, available phosphorus and available potassium in Heyang County were studied The suitability distribution of the indicators, using stepwise regression and path analysis methods, analyzes the direct relationship between soil pH and soil nutrients, and provides a theoretical basis for improving the newly added cultivated land. The results showed that the soil pH in Heyang County varied from 8.42 to 9.67, the soil organic matter content varied from 3.46 to 17.93 g/kg, the soil total nitrogen content varied from 0.13 to 5.61 g/kg, and the soil available phosphorus changed The range is 1.73 ~ 63.06 mg/kg, and the soil available potassium range is 46.50 ~ 523.74. The newly added soil has a certain nutrient basis, but it should be further adjusted and improved during the cultivation process. The direct positive effect on soil pH value is mainly soil organic matter, and the direct negative effect is mainly soil available phosphorus. By adjusting the organic matter, total nitrogen, available phosphorus and available potassium in the soil, the pH value of the soil can be effectively improved, so that the newly cultivated soil is suitable for the growth of local crops.

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