scholarly journals TINGKAT KESUBURAN TANAH PADA AREAL EKS PENEBANGAN HUTAN DI AREAL HPH PT. KSK NANGA PINOH KAB. MELAWI

2018 ◽  
Vol 8 (1) ◽  
Author(s):  
Siti Latifah ◽  
Ratna Herawatiningsih
Keyword(s):  
Organic Matter ◽  
Soil Fertility ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Data Retrieval ◽  
Forest Harvesting ◽  
Survey Method ◽  
Physical And Chemical Properties ◽  
Physical And Chemical ◽  
And Chemical Properties

Forest harvesting is a logging activity, distribution of trunks, skidding, loading and transportation. This activity involves a lot of heavy equipment that results in soil compaction and reduced vegetation cover. This condition causes changes in soil fertility conditions. This study aims to determine changes in soil fertility that occur due to forest exploitation activities. Namely by observing the physical and chemical properties of the soil in the area of the former skid trail, ex-TPn, former TPk, former logging areas. The research method used for data retrieval is the survey method with porposive sampling, while the data obtained is analyzed using descriptive analysis. Based on the results of the analysis of the physical and chemical properties of the soil, it shows that the former TPN area is the area with the lowest soil fertility value. Former logging areas have the best quality of soil fertility compared to other areas; such as former skid trails, former TPk and former Tpn areas even though they are still included in the low fertility classification, with organic matter in the former logged area of 2.24%. The organic matter content is only 0.8% with clay texture.Keyword: harvesting, forest, forest land, soil fertility

scholarly journals Impact of Wastes on Some Properties of Soil around an Active Dumpsite in Ibadan, Southwestern Nigeria

2021 ◽  
Vol 8 (3) ◽  
pp. 27-40
Author(s):  
Oluwatoyin Opeyemi Akintola ◽  
Gabriel Oladapo Adeyemi ◽  
Oluwayemisi Samuel Olokeogun ◽  
Idayat Adewunmi Bodede
Keyword(s):  
Organic Matter ◽  
Soil Organic Matter ◽  
Bulk Density ◽  
Soil Texture ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Available Phosphorus ◽  
Physical And Chemical Properties ◽  
Physical And Chemical ◽  
And Chemical Properties

Recently most farmers in developing country like Nigeria has resulted to the use of solid wastes as compost to replenish the deteriorated soils while some are farming on the abandoned waste dumpsite due to their richness in organic matter. This study assessed the soil nutrient and fertility status by investigating the influence of wastes (if any) on physical and chemical properties of soils in and around Lapite dumpsite for environmental sustainability. Ten soil samples each collected from three locations: dumpsite, downslope and upslope sites at depth of 0-20cm were analyzed for soil texture, bulk density, porosity, electrical conductivity, pH, organic carbon, organic matter content (OMC), total nitrogen (TN), available phosphorus (AP), Na, K, Ca, Mg, Fe, Zn, Cu, Pb and Ni. Significant differences were observed on soil physical: moisture content (18.05-38.11 %); Bulk density (1.01-1.54 g/cm3); porosity (49.09-74.56 %) and chemical properties: : OMC (1.39-5.98 %);TN (0.58-1.60 %); AP(0.35-1.09 %) among others in soils from the studied location sites at p ≤ 0.05; however, no remarkable impact was noticed on soil texture. This study has shown that deposition of wastes has impacted the physical and chemical properties by improving soil organic matter contents and increasing nutrient contents such as exchangeable bases and micronutrient, thus enhancing soil organic matter, fertility and productivity status of the soil for maximum plant growth. However, increase in heavy metal concentrations in dumpsite soils call for incessant assessment and monitoring, thus sorting, reuse and recycling should be encouraged to reduce the metal loads over time.

The Physicochemical Properties of Soils in Tea Gardens Affected by Vermicompost and Lime Applications During Different Time Periods

2021 ◽  
Vol 47 (1) ◽  
pp. 82-94
Author(s):  
Mahmoud Shabanpour ◽  
Azadeh Sedaghat ◽  
Parvin Rousta ◽  
Reza Ebrahimi ◽  
Ahmad Shirinfekr
Keyword(s):  
Organic Matter ◽  
Bulk Density ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Infiltration Rate ◽  
Carbonate Content ◽  
Physical And Chemical Properties ◽  
Significant Difference ◽  
Physical And Chemical ◽  
And Chemical Properties

The organic matter content has significantly decreased in some of the tea gardens in north of Iran, thereforeresulting in degradation of their physical and chemical properties. An experiment was conducted in two tea gardens in order to investigate the effect of lime and vermicompost on soil's physical and chemical properties. The studied tea soils were located in Gilan province (Bazkiyagorab and Azbaram) in Iran (with clay loam and sandy loam texture). Vermicompost was applied in 3 levels of 0, 2.5% and 5% and lime was applied in two levels of 0 and 0.5%. The measurements were carried out three times (after 0, 90 and 180 days). The results showed that lime and vermicompost application has significantly affected the calcium carbonate content, pH, the electrical conductivity (EC) and the soil organic matter (SOM) content in the studied soils. Lime application significantly increased the infiltration rate (P<0.01). Comparison of the average interaction of lime with vermicompost in the Azbaram station soil showed that 5% vermicompost and 0.5% lime with an average of 5.49 (mm h-1) had the highest infiltration rate (IR) and had a significant difference with the other treatments. Comparison of the average interaction of lime with vermicompost in Basquegorob garden showed that the treatment of 5% vermicompost with 0.5% lime, the time stage of 180 days with an average density of 1.11 (g cm-3) had the lowest bulk density (BD) and was significantly different from other levels. It seems that the simultaneous presence of lime and vermicompost and their effect on improving the soil structure and increasing porosity, leads to reduction of the soil's bulk density. The results obtained in this study have clearly indicated that the simultaneous applications of vermicompost and lime is an effective way to improve soil physical and chemical properties. However, the real potential of the amendments used in this experiment should be further assessed under field conditions using a test crop.

scholarly journals Physical and Chemical Properties of Soil in the Sahelian Region: Case Study in Nioro du Rip, Senegal

2020 ◽  
pp. 73-82
Author(s):  
Landing Biaye ◽  
Fary Diome ◽  
Seybatou Diop ◽  
Modou Mbaye ◽  
Djibril Tine ◽  
...  
Keyword(s):  
Agricultural Land ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Principal Component ◽  
Fertility Level ◽  
Physical And Chemical Properties ◽  
Limited Information ◽  
Geochemical Composition ◽  
Physical And Chemical ◽  
And Chemical Properties

The locality of Nioro du Rip is facing intense erosion, loss of agricultural land, soil pollution and soil degradation. Today, there is limited information about the soil physical and chemical properties in the locality. In this work, we describe the main essential factors or mechanism that control the evolution of the soil in the study area. The physical and chemical properties of soils encountered along a NE-SW transect in are analyzed in this paper. The statistical analysis results revealed low structural stability of soils in general, due to their low organic matter content and exchangeable bases and their predominantly silty texture. A net trend towards acidification, which is more pronounced in the lower-bottom and terrace soils, provides information on the conditions that are increasingly unfavorable to agricultural development. The multivariate principal component analysis (PCA) identified the preponderance of two factors among the four primarily involved in soil geochemical composition. These include a mineralization process (expressed through the first principal component (PC1), which causes soils to be rich in elements (Ca2+, K+,C, N, MO) controlling their structure and fertility level;  The PC2 axis expresses the spatial differentiation phenomenon of the soil granulometric composition: soils forming cluster poles according to their textural affinity in the projection of the plane formed by these two components , with on one side the sandy-dominated soils of the shallows and terraces and on the other the clay-dominated soils of the plateau and the slope. A clear reversal of textural polarity in the studied topo sequence that must be blamed on the strong water erosion in this area.

scholarly journals Physical properties and particle-size fractions of soil organic matter in crop-livestock integration

2012 ◽  
Vol 36 (4) ◽  
pp. 1299-1310 ◽  
Author(s):  
Carolina Tirloni ◽  
Antonio Carlos Tadeu Vitorino ◽  
Anderson Cristian Bergamin ◽  
Luiz Carlos Ferreira de Souza
Keyword(s):  
Organic Matter ◽  
Soil Quality ◽  
Crop Rotation ◽  
Cover Crops ◽  
Chemical Properties ◽  
Environmental Stability ◽  
Native Forest ◽  
Physical And Chemical Properties ◽  
Physical And Chemical ◽  
And Chemical Properties

Crop-livestock integration represents an interesting alternative of soil management, especially in regions where the maintenance of cover crops in no-tillage systems is difficult. The objective of this study was to evaluate soil physical and chemical properties, based on the hypothesis that a well-managed crop-livestock integration system improves the soil quality and stabilizes the system. The experiment was set up in a completely randomized design, with five replications. The treatments were arranged in a 6 x 4 factorial design, to assess five crop rotation systems in crop-livestock integration, and native forest as reference of soil undisturbed by agriculture, in four layers (0.0-0.05; 0.05-0.10; 0.10-0.15 and 0.15-0.20 m). The crop rotation systems in crop-livestock integration promoted changes in soil physical and chemical properties and the effects of the different systems were mainly detected in the surface layer. The crops in integrated crop-livestock systems allowed the maintenance of soil carbon at levels equal to those of the native forest, proving the efficiency of these systems in terms of soil conservation. The systems influenced the environmental stability positively; the soil quality indicator mineral-associated organic matter was best related to aggregate stability.

Composting winery wastes with clinoptilolite. Suitability for land application.

2020 ◽  
Author(s):  
Chronis Kolovos ◽  
Maria Doula ◽  
Stamatios Kavasilis ◽  
Georgios Zagklis ◽  
Gerasimos Tsitselis ◽  
...  
Keyword(s):  
Electrical Conductivity ◽  
Organic Matter ◽  
Agricultural Waste ◽  
Organic Fertilizer ◽  
Chemical Properties ◽  
Land Application ◽  
Physical And Chemical Properties ◽  
Physical And Chemical ◽  
Winery Waste ◽  
And Chemical Properties

&lt;p&gt;Soil application of raw winery wastes is a procedure of doubtful appropriateness, mainly because of waste properties, i.e. very acidic pH; high electrical conductivity; and high content of polyphenols. The disposal of winery waste on soils may cause various environmental and health hazards as for example soil overloading with polyphenols and salts, phytotoxicity to plants, odor nuisance etc. Pathogens, which may still be present in the decomposed material could spread plants and soil diseases, while waste piles attract insects, pests, domestic rodents and wildlife which may threaten public and animal health. Despite these facts, many wine producers discharge winery waste to the nearby agricultural or forest ecosystems, without treatment although this type of agricultural waste could be a significant source of organic matter and nutrients.&lt;/p&gt;&lt;p&gt;&amp;#160;&lt;/p&gt;&lt;p&gt;In general, degradation of winery waste is a slow procedure which becomes even slower under the xerothermic climatic conditions in Greece, which may slow down the microbially mediated decomposition of organic matter and nutrients cycling; degradation of winery waste piles takes more than 5 years to be completed naturally. However, the final products are of doubtful appropriateness for fertilization use, mainly because of low quality organic matter and low nutrients content (lost mainly due to the exposure of piles to uncontrolled environmental conditions for years).&lt;/p&gt;&lt;p&gt;&amp;#160;&lt;/p&gt;&lt;p&gt;This study aims to highlight the advantages of composting winery wastes by using also other agricultural wastes and additives as feedstock to produce a safe and environment friendly compost, appropriate for application to agricultural ecosystems. For this a 41 hectares vineyard in North Greece of about 400 tn grapes yield annually and generation of approximately 100 tn of waste was selected. Winery waste was collected after harvesting and wine-making period of 2018 and composted with cow manure, wheat straw and clinoptilolite up to 5%.&lt;/p&gt;&lt;p&gt;&amp;#160;&lt;/p&gt;&lt;p&gt;Composting phase lasted 5 months, and during this period the pile was monitored as regard temperature, moisture and oxygen content. After composting completion, the final product was fully characterized in terms of its physical and chemical properties, considering national legislation organic materials reuse on soils. The outcomes of this study show a great potential for managing such waste types by composting using clinoptilolite in the feedstock materials since the final product has suitable physical and chemical properties for many crops, i.e. slight alkaline pH, low electrical conductivity, low polyphenol content and high content of available nutrient, therefore can be used as soil amendment or organic fertilizer.&lt;/p&gt;

Control of soil development on the Tanana River floodplain, interior Alaska

1993 ◽  
Vol 23 (5) ◽  
pp. 941-955 ◽  
Author(s):  
K. Van Cleve ◽  
C.T. Dyrness ◽  
G.M. Marion ◽  
R. Erickson
Keyword(s):  
Particle Size ◽  
Organic Matter ◽  
Surface Soil ◽  
Chemical Properties ◽  
Physical And Chemical Properties ◽  
Vegetation Development ◽  
River Floodplain ◽  
Soil Particle Size ◽  
Physical And Chemical ◽  
And Chemical Properties

Alluvial soils on the Tanana River floodplain near Fairbanks, Alaska, were examined for development of physical and chemical properties in relation to soil depth and across a 200-year vegetation development sequence. Development was mediated by ecosystem controls including successional time, vegetation, terrace height, soil physical and chemical properties, and microclimate. These controls interact and are conditioned by the state factors time, flora, topography, parent material, and climate, respectively. On early-successional (<5 years) lower alluvial surfaces, terrace height above groundwater, soil particle size, and microclimate (through soil surface evaporation) interacted through capillary rise to produce salt-affected surface soil. Calcium salts of carbonate and sulfate were the principal chemicals encountered in these soils. Establishment of a vegetation cover between 5 and 10 years introduced evapotranspiration as a new mechanism, along with capillarity, to control moisture suction gradients. In addition, newly formed surface litter layers further helped eliminate evaporation and formation of high salt content surface soil. Continued sedimentation raised terrace elevation, so on older terraces only infrequent flood events influenced soil development. Moreover, in these successional stages, only the highest river stages raised groundwater levels, so transpiration and capillarity influenced water movement to tree root systems. During the first 25–30 years of succession, plant deposition of organic matter and nitrogen, associated with the growth of alder, markedly changed soil properties. Nearly 60% (or 240 g•m−2) of the 400 g•m−2 nitrogen encountered at 100 years was accumulated during this early period. After 100 years of vegetation development, soil carbonate content dropped to about half the peak values of about 1600 g•m−2 encountered between 4 and 25 years. By the time white spruce was the dominant forest type at 180 years, carbonate carbon declined to about 500 g•m−2, one-third that of the 1600 g•m−2 high. By this time surface soil pH declined from high values of 7.5 to between 5.5 and 6.0. Organic carbon continued to accumulate to about 6300 g•m−2 in the white spruce stage, twice that encountered in the alder–poplar stage at 25 years. Indices of moisture retention were most strongly related to either soil particle size (low moisture tension and available moisture range) or vegetation-mediated soil organic matter content (high moisture tension). Cation exchange capacity was most strongly related to a vegetation-mediated index of organic matter (OM) content (%N, %C, or %OM).

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 PRODUÇÃO E CARACTERIZAÇÃO DE BIOCARVÃO A PARTIR DE BIOSSÓLIDOS ARMAZENADOS EM BAG’s GEOTÊXTEIS NO MUNICÍPIO DE RANCHARIA -SP

2019 ◽  
Vol 11 (4) ◽  
pp. 142-155
Author(s):  
Beatriz Regina de Ângelo ◽  
Rafaela Pelegrini Vital ◽  
Marcelo Rodrigo Alves ◽  
Jaqueline Oliveira da Silva ◽  
Melissa Arantes Pinto ◽  
...  
Keyword(s):  
Organic Matter ◽  
Sewage Sludge ◽  
Chemical Properties ◽  
Physical And Chemical Properties ◽  
Pyrolysis Process ◽  
Physical Chemical ◽  
Physical And Chemical ◽  
Stable Material ◽  
And Chemical Properties

Sewage sludge refers to a nutrient-rich by-product and organic matter from treatment plants and has become a challenge for many research segments to find a rational and sustainable destination for this material. In this context, the carbonization of biomass (by the pyrolysis process) results in biochar, characterized by a very stable material with specific physical and chemical properties and can represent a very important tool for this challenge. Thus, the objective of the present work was to transform, bypyrolysis process, small portions of the biosolid generated in Rancharia ETE into biochar. In addition, both the biosolid and the generated bicarbons were subjected to physical, chemical and structural analyzes in order to proceed with their respective characterization. From the analysis, it was found that the treatment submitted to temperature of 550°C as the best option for possible applications.Keywords:biosolid; pyrolysis; biochar.

GENESE D’UN HORIZON PROFOND FAIBLEMENT CIMENTE DANS UN PODZOL SABLEUX DES BASSES TERRES DU QUEBEC

1979 ◽  
Vol 59 (2) ◽  
pp. 105-117 ◽  
Author(s):  
F. PAGE ◽  
M. ROMPRE ◽  
G. A. BOURBEAU ◽  
C. R. DE KIMPE
Keyword(s):  
Organic Matter ◽  
Chemical Properties ◽  
Relative Content ◽  
Physical And Chemical Properties ◽  
Iron Aluminum ◽  
Sandy Deposit ◽  
Physical And Chemical ◽  
Micromorphological Analysis ◽  
And Chemical Properties

An Orthic Humo-Ferric Podzol formed on a sandy deposit in the St. Lawrence lowlands exhibited a weakly cemented horizon at depth. Weathering of minerals was active mainly in the upper Ae horizon and released large amounts of iron, aluminum and silica. These elements migrated down the profile as organo-metallic complexes and accumulated as concretions in the podzolic B-horizons but also in the cemented horizon at depth. Micromorphological analysis showed that this latter horizon had a chlamydic/plectic assemblage. A comparison was made with other horizons found at depth in various profiles and differing from this one by their macro- and micromorphological, physical and chemical properties. The relative content of the various constituents of the cement was calculated. The sum of organic matter plus free sesquioxides ranged from 7 to 85%. There are apparent similarities in the formation of ortstein and duric horizons. The results serve to establish the concept of "ortstein-duric horizon-fragic horizon" intergrades in weakly cemented horizons found at depth in many Quebec soils.

The Impact of Different Grazing Intensity on Topsoil Physical and Chemical Properties in Xilamuren Grassland

2013 ◽  
Vol 295-298 ◽  
pp. 2090-2096
Author(s):  
Yi Fang ◽  
Xiao Jia Li ◽  
Cong Cong Chen ◽  
Min Zhang ◽  
Rui Ping Zhou ◽  
...  
Keyword(s):  
Particle Size ◽  
Organic Matter ◽  
Soil Organic Matter ◽  
Chemical Properties ◽  
Grazing Intensity ◽  
Physical And Chemical Properties ◽  
Grassland Ecosystem ◽  
The Difference ◽  
Physical And Chemical ◽  
And Chemical Properties

Grassland is an important ecosystem in land surface. Soil is the basis of grassland ecosystem, and the changes of its properties directly affect grassland ecosystem. The study region is located in Xilamuren grassland using the methods of field sampling and experimental analysis. It was divided into four test areas according to grazing intensity. Soil physical and chemical properties were analyzed in each test area. The results showed that: the trend of soil water content decreased and then increased with increasing grazing intensity, soil water content in repaired grassland was the lowest. For the soil mechanical composition, particle size content increased first and then decreased with increasing grazing intensity when the particle size was 1-0.05mm. The difference between the highest and lowest values was obvious. When the particle size was 0.05-0.002mm, the trend of particle size fluctuated, first decreased and then increased, finally reduce again and the difference between the highest and lowest values was obvious. When the particle size was less than 0.002mm, the trend of particle size content increased with increasing grazing intensity. In soil chemical properties, soil organic matter appears downward trend overall as grazing intensity increase. Soil organic matter content was the lowest in repaired grass. Available N and P first decreased and then increased with increasing grazing intensity, the minimum values appeared in the repaired grassland and degraded grassland respectively. Available K content increased with increasing grazing intensity.

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