scholarly journals The Combined Effect of Biochar and Mineral Fertilizer on Triticale Yield, Soil Properties under Different Tillage Systems

Plants ◽  
2021 ◽  
Vol 11 (1) ◽  
pp. 111
Author(s):  
Luiza Usevičiūtė ◽  
Edita Baltrėnaitė-Gedienė ◽  
Dalia Feizienė
Keyword(s):  
Soil Properties ◽  
Sandy Loam ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Mineral Fertilizer ◽  
Matter Content ◽  
Npk Fertilizers ◽  
Physical Chemical ◽  
Tillage System ◽  
Direct Drilling

This study examined the effect of study time, biochar dose, and fertilization-tillage system on the improvement of sandy loam physical-chemical properties and triticale grain yield. The soil properties (water holding capacity (WHC), wettability, moisture content (MC), organic matter content (SOM), pH, and electrical conductivity (EC) were monitored in short time intervals (after 3, 6, 12, and 24 months). Soil was tilled in two methods (shallow ploughless tillage and direct drilling), fertilized with nitrogen, phosphorus, and potassium (NPK) fertilizers, and amended with three hydrophobic pine wood biochar doses (0 t/ha; 5 t/ha; 15 t/ha). It was found that 15 t/ha biochar dose had the highest effect on the soil’s physical-chemical properties improvement (SOM increased by 33.7%, pH—by 6.84%, EC—by 23.4%, WHC—by 8.48%, and MC—by 21.8%) compared to the variants without biochar. Direct drilling, fertilization with NPK fertilizers and 15 t/ha biochar dose significantly influenced the rise of soil’s physical-chemical properties and triticale yield (3.51 t/ha).

scholarly journals Effects of freeze-thaw on soil properties and water erosion

2021 ◽  
Author(s):  
Baoyang Sun ◽  
Feipeng Ren ◽  
Wenfeng Ding ◽  
Guanhua Zhang ◽  
Jinquan Huang ◽  
...  
Keyword(s):  
Soil Moisture ◽  
Soil Erosion ◽  
Soil Properties ◽  
Field Experiments ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Water Erosion ◽  
Matter Content ◽  
Experimental Conditions ◽  
Freeze Thaw

Freeze-thaw erosion occurs primarily at high latitudes and altitudes. Temperature controlled freeze-thaw events dislodge soil particles and serve as a catalyst for erosion. This review paper provided an overview of the effects of freeze-thaw on soil properties and water erosion. The process of freeze-thaw cycles results in temporary and inconsistent changes in the soil moisture, and affects the soil’s mechanical, physical and chemical properties, such as the soil moisture content, porosity, bulk density, aggregates stability, shear strength and organic matter content and so on. The variation trend and range of the soil properties were related to the soil texture, water content and freeze-thaw degree. Furthermore, the soil erosion was affected by the freeze-thaw processes, as thawing and water erosion reinforce each other. However, research of different experimental conditions on indoor simulations have numerous limitations compared with field experiments. The use of indoor and field experiments to further reveal the freeze-thaw effect on the soil erosion would facilitate improved forecasting.

scholarly journals HUBUNGAN KESUBURAN TANAH DENGAN PRODUKTIVITAS TANAMAN

Jurnal Solum ◽  
2010 ◽  
Vol 7 (1) ◽  
pp. 27
Author(s):  
Asmar Asmar ◽  
Amrizal Saidi ◽  
Masliyunas Masliyunas
Keyword(s):  
Physical Properties ◽  
Soil Properties ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Gravimetric Method ◽  
Crop Productivity ◽  
Soil Physical Properties ◽  
Matter Content ◽  
Soil Samples ◽  
Organic C

A research about relationship between soil properties and crop yield was conducted in Pandai Sikek, Tanah Datar Region, center for cabbage and carrot production, West Sumatra in 2004 and 2005.  Soil samples were collected from rainfed paddy soils by purposive random sampling.  Soil samples were analyzed in Soil Laboratory, Agriculture Faculty and Agriculture Polytechnique Laboratory, Andalas University.  Several soil physical properties analysed were soil bulk density and total soil pores by using gravimetric method, permeability with de Boodt method, soil water content at several pF values using pressure plate apparatus, and soil strength by using penetrometer.   Soil chemical parameters analysed were soil pH using pH-meter, organic-C using Walkley and Black, available P using Bray II, and cation exchange capacity using NH4-leaching at pH 7.0, and N-total using Kjehdhal method.  Crop productions were sampled from a 3x3 m2 of soil sampling area.  The result showed that soils planted by cabbage and carrot had good soil physical properties, such as having balanced pore size distribution.  The chemical properties of the soils were good as well, except N, K- and Ca-exchangeable which were very low.  The other soil properties were quite good.  Soil physical properties gave different response on both crops.  Carrots were more response aeration pore and soil organic matter content, then cabbage was more response on BV, TSP, and slow drainage pores.  While soil chemical properties did not give significant response.  Both crops responded on Ca, but cabbage was more response on N-total, and carrot on CEC and saturated cationKey Words: Soil Physical Properties, Soil Fertility, Crop Productivity

scholarly journals Municipal Sewage Sludge application on cotton cultivations. Effect on yields soil chemical properties and heavy metal concentrations

2019 ◽  
Keyword(s):  
Sewage Sludge ◽  
Soil Properties ◽  
Agricultural Soils ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Matter Content ◽  
Municipal Sewage ◽  
Municipal Sewage Sludge ◽  
Available Phosphorus ◽  
Cotton Yield

<p>Application of municipal sewage sludge (MSS) to agricultural soils is a current practice in EU. European legislation permits its use in agriculture when concentrations of metals in soil do not exceed the maximum permissible limits. In order to study the influence of MSS on cotton yield and soil properties, a filed experiment was conducted in a soil classified as Typic Xerochrepts located in Lamia area, central Greece, for two consecutive years. The experimental design was complete randomized blocks with four treatments: Control (C ), inorganic fertilization (IF), application of 6000 dry kg ha-1 MSS, and 10000 dry SS kg ha-1, each replicated 4 times. The results showed that MSS application in both rates, increased significantly cotton yield compared to control equally to inorganic fertilization. Soil properties, at the end of the second year of MSS application, were significantly affected by MSS application in a positive way i.e. pH decreased slightly, but organic matter content, available phosphorus, total nitrogen concentrations exchangeable potassium and available zinc and copper increased significantly. The potentially toxic elements lead, chromium, and nickel were not significantly affected by MSS application in both application rates compared to control.</p>

scholarly journals Biological and Physicochemical Parameters Related to the Nitrogen Cycle in the Rhizospheric Soil of Native Potato (Solanum phureja) Crops of Colombia

2011 ◽  
Vol 2011 ◽  
pp. 1-10
Author(s):  
Nathalia Flórez-Zapata ◽  
Daniel Uribe-Vélez
Keyword(s):  
Organic Matter ◽  
Nitrogen Cycle ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Matter Content ◽  
Solanum Phureja ◽  
Rhizospheric Soil ◽  
Nitrogen Fixing ◽  
Nitrogen Fixing Bacteria ◽  
Physical Chemical

Nitrogen (N) plays an important role in agricultural production. This study was designed to evaluate the presence of cultivable N cycle-associated microorganisms (nitrogen-fixing bacteria—NFB, proteolytic bacteria—PR, ammonifiers—AMO, ammonium-oxidizing bacteria—AOB, nitrite-oxidizing bacteria—NOB, and denitrifiers—DEN), and their relationship with physical-chemical and agronomic soil descriptors, inSolanum phurejarhizospheric soil samples, from traditional and organic crop management farms. A cluster analysis with the physical and chemical properties of soil, allowed to identify the organic matter content as an important factor that determines the outcome of that grouping. Significant differences () between farms were found in the abundance of this groups, but correlation analysis showed that proteolytic and nitrogen fixing bacteria were the main nitrogen associated functional groups affected by soils' physical-chemical characteristics. The amount of ammonia available is affected by the agricultural management strategy, which consequently affects the NFB abundance. Finally the results showed that PR, protease activity and soil properties related with organic matter transformation has a positive relationship with productivity, which given the high organic matter content of the Andean soils being studied, we conclude that nitrogen mineralization process has an important role in the nitrogen cycle and its bioavailability in this ecosystem.

Decomposition of plant material in Australian soils .IV. Decomposition in situ of 14C labeled and 15N labeled legume and wheat materials in a range of southern Australian soils

Soil Research ◽  
1987 ◽  
Vol 25 (1) ◽  
pp. 95 ◽  
Author(s):  
M Amato ◽  
JN Ladd ◽  
A Ellington ◽  
G Ford ◽  
JE Mahoney ◽  
...  
Keyword(s):  
Organic Matter ◽  
Soil Properties ◽  
Wheat Straw ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Matter Content ◽  
Organic N ◽  
Root Decomposition ◽  
Plant Materials ◽  
Organic C

14C- and 15N-labelled wheat straw, and tops or roots of a pasture legume (either Medicago littoralis or Trifolium subterraneum) were incorporated into topsoils at 12 field sites in southern Australia. These sites were representative of soil types widely used for wheat growing in each region. The soils varied markedly in their physical and chemical properties (e.g. pH, texture and organic matter content). Based on amounts of residual I4C (averaged for all sites), the legume tops decomposed more extensively than did wheat straw, especially soon after incorporation. To a lesser extent the legume tops decomposed more extensively than legume roots, and T. subterraneum tops more than M. littoralis tops; root decomposition for both legumes was similar. For example, after 1 year, the residual organic 14C from wheat straw, M. littoralis tops, T. subterraneum tops and legume roots accounted for 48%, 41%, 38% and 54% of their respective inputs. After two years, residual 14C of wheat straw accounted for 30% of the input. Differences in decomposition due to climate and soil properties were generally small, but at times were statistically significant; these differences related positively with rainfall and negatively with soil clay content, but showed no relationship with pH or soil organic C and N. Some N was mineralized from all plant materials, the greatest from legume tops, the least from wheat straw. After 1 year, residual organic 15N accounted for 56%, 63% and 78% respectively of input l5N from legume tops and roots and from wheat straw. The influence of climate and soil properties on amounts of residual organic I5N was small and generally was consistent with those found for residual 14C. AS an exception, the residual organic 15N from wheat straw was negatively related to soil organic N levels, whereas residual I5N of legume tops and roots and residual 14C of all plant materials were not influenced by soil organic matter levels. These results are discussed in terms of the turnover of N in soils amended with isotope labelled plant materials of different available C:N ratios.

scholarly journals Assessment of Soil Properties Under Different Land Use Types in Olokemeji Forest Reserves in Ogun State Southwestern Nigeria

2020 ◽  
Vol 7 (3) ◽  
pp. 73-84
Author(s):  
OLUWATOYIN OPEYEMI AKINTOLA ◽  
ADEWUNMI IDAYAT BODEDE ◽  
MICHAEL MICHAEL ◽  
AYODEJI GIDEON ADEBAYO ◽  
OLAWALE NUREAN SULAIMAN
Keyword(s):  
Soil Properties ◽  
Environmental Sustainability ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Matter Content ◽  
Natural Forest ◽  
Available Phosphorus ◽  
Forest Plantation ◽  
Southwestern Nigeria ◽  
Significant Difference

Knowledge of soil properties is essential for environmental sustainability for any forest reserve or plantation. The physical and chemical properties of soil under three different land uses was investigated to assess the nutrient and fertility status of the soils. Fifteen soil samples, each collected from different locations within the natural forest, plantation and farm land were analyzed for soil texture, bulk density, porosity, pH, organic carbon, organic matter content, total nitrogen, available phosphorus, Na, K, Ca, Mg, Zn, Cu, Fe and Mn. Texturally, the soils were loamy, loamy sand and sandy loamy in the natural forest, plantation and farmland respectively. There was a significant difference between the three different soils in composition and texture.

scholarly journals Soil biochemical response after 23 years of direct drilling under a dryland agriculture system in southwest Spain

2008 ◽  
Vol 147 (1) ◽  
pp. 9-15 ◽  
Author(s):  
S. MELERO ◽  
K. VANDERLINDEN ◽  
J. CARLOS RUIZ ◽  
E. MADEJÓN
Keyword(s):  
Alkaline Phosphatase ◽  
Conservation Tillage ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Principal Component ◽  
Soil Surface ◽  
Farming System ◽  
Biochemical Properties ◽  
Matter Content ◽  
Direct Drilling

SUMMARYSoil enzyme activities are widely utilized as rapid and sensitive indicators in discriminating among soil management effects. The objective of the present study was to compare the influence of conservation tillage, i.e. direct drilling (DD) (residue cover is left on the soil surface)v. conventional tillage (CT), on soil chemical and biochemical properties in a crop rotation (cereals–sunflower–legumes) under dryland production in a semi-arid Mediterranean Vertisol after 23 years. A randomized experimental design was established. Soil biological status was evaluated by measuring of enzymatic activities (dehydrogenase, β-glucosidase, alkaline phosphatase and protease). Total organic carbon (TOC) contents were greater in soils managed by DD than those found by CT. Except for protease activity, enzymatic activity values were approximately 2-fold higher in soils under DD than in soils under CT. The β-glucosidase, alkaline phosphatase and dehydrogenase values showed a high correlation (fromr=0·481 tor=0·886,P⩽0·01) with TOC contents and they were correlated with each other (fromr=0·664 tor=0·923,P⩽0·01). The coefficient of variation of biochemical properties was higher than those of chemical properties in both treatments. Principal component analysis (PCA) showed that two principal components explained 58% and 20% of the total variability. The first principal component was influenced mostly by β-glucosidase, dehydrogenase and TOC, whereas the second was influenced by pH. The first component effectively differentiated managed soil under both agriculture practices. In general, long-term soil conservation management by DD in a dryland farming system improved the quality of this Vertisol by enhancing its organic matter content and biochemical activity.

Wildfire temperature effect on soils physical and hydraulic properties

2020 ◽  
Author(s):  
Sofía Martínez ◽  
Cristina Contreras ◽  
Sara Acevedo ◽  
Carlos Bonilla
Keyword(s):  
Hydraulic Conductivity ◽  
Soil Properties ◽  
Soil Water ◽  
Hydraulic Properties ◽  
Sandy Loam ◽  
Organic Matter Content ◽  
Matter Content ◽  
Burned Area ◽  
Laboratory Procedure ◽  
Natural Fire

&lt;p&gt;Wildfires affect soil physical, chemical, and hydraulic properties, which in turn control many processes such as soil water availability, soil water balance, infiltration, and soil stability. Because of the multiple factors controlling the changes in soil properties and the nature of fire events, the number of predictive models for these effects is limited. Therefore, the objective of this study was to develop a soil-burning laboratory procedure to identify changes in physical and hydraulic soil properties across a fire temperature range. With this purpose, saturated hydraulic conductivity, pH, electric conductivity, soil texture, aggregate stability, repellency, and organic matter content (OM) were measured in soils burned at increasing temperatures. Six sandy loam soils were burned at four different temperatures (300&amp;#186;C, 500&amp;#186;C, 700&amp;#186;C and 900&amp;#186;C) and non-burned samples were used as a control to compute the change on each property. Additionally, three of these soils were sampled in a naturally burned area and used later to test the laboratory setup reliability to reproduce a natural fire. Preliminary results for soils burned in a muffle furnace (300&amp;#186;C for two hours) showed that the changes in physical properties are more significant with soils rich in OM. On the other hand, properties such as water retention and hydraulic conductivity curves showed little variation at 300&amp;#186;C.&lt;/p&gt;

scholarly journals Physical and Chemical Properties of Soils in Gambari Forest Reserve Near Ibadan, South Western Nigeria.

2020 ◽  
Vol 7 (2) ◽  
pp. 57-67 ◽  
Author(s):  
Akintola Opeyemi ◽  
Bodede Adewunmi ◽  
Abiola Oluwaseyi
Keyword(s):  
Organic Matter ◽  
Bulk Density ◽  
Total Nitrogen ◽  
Sandy Loam ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Matter Content ◽  
Available Phosphorus ◽  
Forest Reserve ◽  
Physical And Chemical

The different features of soil greatly affect the flora and vegetative diversity of a forest. The physical and chemical characteristics of soils in Onigambari Forest Reserve were evaluated to assess the fertility and productivity status of the soils. Fifteen soil samples collected from different sample locations were analyzed for soil texture (sand, silt and clay), bulk density, porosity, pH, organic matter, total nitrogen, available phosphorus, exchangeable bases (Na, K, Ca and Mg) and available micronutrients (Zn, Cu, Fe and Mn). Texturally, the studied soils were loamy sand and sandy loam with percentage of sands (71.2-84.2 %), silts (7.4-10.4 %) and clay (6.4-19.4 %). The bulk density of the soils was 1.61-1.83 % while the porosity of the soils ranged from 35.2-44.1 %. The slightly acidic to neutral soil pH (5.90 - 6.60) and medium organic matter content (1.68 -2.60 %) suggest adequate level of soil nutrients. The soils had high total nitrogen (0.35 -0.65 %) and available phosphorus contents between 10.98 and 18.22mg/kg.

Physico-Chemical Properties of Soil Collected from Chandrabhaga River in Kalmeshwar, Nagpur, Maharashtra

2020 ◽  
Vol 07 (02) ◽  
pp. 1-3
Author(s):  
Amita M Watkar ◽  
Keyword(s):  
Organic Matter ◽  
Soil Quality ◽  
Agricultural Land ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Matter Content ◽  
Soil Attributes ◽  
Essential Components ◽  
Agricultural Land Management ◽  
Physical And Chemical

Soil, itself means Soul of Infinite Life. Soil is the naturally occurring unconsolidated or loose covering on the earth’s surface. Physical properties depend upon the amount, size, shape, arrangement, and mineral composition of soil particles. It also depends on the organic matter content and pore spaces. Chemical properties depend on the Inorganic and organic matter present in the soil. Soils are the essential components of the environment and foundation resources for nearly all types of land use, besides being the most important component of sustainable agriculture. Therefore, assessment of soil quality and its direction of change with time is an ideal and primary indicator of sustainable agricultural land management. Soil quality indicators refer to measurable soil attributes that influence the capacity of a soil to function, within the limits imposed by the ecosystem, to preserve biological productivity and environmental quality and promote plant, animal and human health. The present study is to assess these soil attributes such as physical and chemical properties season-wise.

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