scholarly journals Soil physicochemical properties under eucalyptus tree species planted in alley maize cropping agroforestry practice in Decha Woreda, Kaffa zone, southwest Ethiopia

2021 ◽  
Vol 10 (2) ◽  
pp. 7-14
Author(s):  
A Alemayhu ◽  
G Yakob
Keyword(s):  
Physicochemical Properties ◽  
Soil Nutrients ◽  
Tree Species ◽  
Soil Depth ◽  
Rotation Period ◽  
Soil Samples ◽  
Soil Physicochemical Properties ◽  
Total N ◽  
Significant Difference ◽  
Open Land

Different studies have shown that the effect of eucalyptus trees on soil physicochemical properties is variable, which indicates that more investigations that focus on different specific geographical locations and eucalyptus tree species are required. The objectives of this study was to evaluate the status of soil nutrients under four eucalyptus tree species planted in hedgerow system in comparison with that in its adjacent open land. To achieve these objectives, soil samples were taken from a soil depth of 0-20 cm from 15-20 spots by using auger and composited for respective treatments. Each soil samples analyzed at Teppi soil laboratory following standard procedures. Analysis of variance (ANOVA) and treatments separation were made by using Least Significance Difference (LSD) at 95% probability level. The analysis result indicated that there were no significance differences between Eucalyptus tree species and its adjacent open land in the level of soil nutrients (total N, available P, pH, OM, soil moisture and OC) (p<0.05). The only significant difference recorded between Eucalyptus tree species and its adjacent open land in the level of sand percentage whereas non-significant difference was noticed between the treatments on the level of silt and clay percentage in the study. Finally, the results indicate that the eucalyptus tree species established in hedgerow system on clay soil in high rainfall area have no significant impact on soil physicochemical properties under short rotation period of the tree species. Int. J. Agril. Res. Innov. Tech. 10(2): 7-14, December 2020

Soil Physicochemical Properties of Cultivated Land in Different Farming Years in Korqin Sand Land

2012 ◽  
Vol 518-523 ◽  
pp. 4642-4648
Author(s):  
Yong Fang Wang ◽  
Hui Juan Bao ◽  
Chun Xing Hai ◽  
Yin Shan Bao
Keyword(s):  
Physicochemical Properties ◽  
Soil Nutrients ◽  
Soil Texture ◽  
Nutrient Content ◽  
Available P ◽  
Soil Physicochemical Properties ◽  
Cultivated Land ◽  
Total N ◽  
Sand Land ◽  
Windward Slope

Naiman County is the typical area in Korqin sand land. Chose cultivated land in Naiman County, this article carried on comparative analysis for soil physicochemical properties of cultivated land in different farming years. This included change characteristics of soil physicochemical properties with different farming years in different slope positions (windward slope, sloping top and leeward slope) of cultivated land and quantitative analysis between farming years and soil physicochemical properties. The results showed that: (1) there were different changes in soil texture in different slope positions of cultivated land in different farming years: at first 15 years, in the windward slope, the soil texture emerged good trend year by year, but after 30 years of farming, the soil texture get significantly worse. In the sloping top and leeward slope, the soil texture was changed for the better trend along with the increase of farming years. (2)There were different changes in soil nutrients in different slope positions of cultivated land during different farming years: in the windward slope, farmed from 3 years to 15 years, upward trend showed among the most nutrients and until 30 years, it obviously reduced and drop back to level of the 3 years; There was a rising trend in the leeward part of the nutrients; sloping top was between the middle and more indicators decline in nutrient content than that of increasing. (3) There was relationship between the farming years and soil physicochemical properties: the effects on soil texture was higher than the soil nutrients and correlation between different slope positions was different: in the windward slope, farming years correlated positively with sand and available P and a negative correlation was found between farming years and other indicators. In the sloping top, farming years correlated negatively with sand, total N, total K, alkaline N and available P, correlated positively with other indicators. In the leeward slope, farming years correlated negatively only with sand and total K, correlated positively with all of other indicators.

scholarly journals Soil Physicochemical Properties Variation in Black Soil after the Long-term Application of Different Organic Amendments

2020 ◽  
pp. 24-34
Author(s):  
Yaa Opoku-Kwanowaa ◽  
Jinggui Wu ◽  
Xiaodong Chen ◽  
Ahmed Sharaf ◽  
Sonny Gad Attipoe
Keyword(s):  
Organic Matter ◽  
Physicochemical Properties ◽  
Organic Materials ◽  
Organic Amendments ◽  
Black Soil ◽  
Soil Samples ◽  
Chicken Manure ◽  
Soil Physicochemical Properties ◽  
Total N ◽  
Study Results

Aims: This research aimed to assess how the physicochemical properties of black soil respond to different organic amendments after 10 years of application. Study Design: The experiment was established in 2010 and followed a randomized block design consisting of 24 plots (5 m × 5 m) 25 m2 with eight treatments in three replicates. Place and Duration of Study: The study site was located at the Jilin Agricultural University Research Farm, Northeast China (43°48′ N, 125°23′ E; km). Methodology: The treatments for the study included an annual input of chemical fertilizer and organic amendments at the surface of the soil. The treatments were: Control (CK), chicken manure (JM), fodder grass (FG), mushroom (MS), maize straw (MZ), tree leaf (TL), pig manure (PM) and cow manure (CM). Chemical fertilizers were added at the rate of 165 kg of N, 82.5 kg of P and 82.5 kg of K ha_1 per year. Application rates of organic materials were adjusted to similar amounts of organic matter (2000 kgha−1). In June 2019, soil samples were collected from each of the amended fields. In each field, three sampling points were randomly selected. Soil samples were collected from the 0 – 20 cm depth using a core sampler then taken to the laboratory for soil physicochemical properties analysis. Results: Comparing the results of the organic treatments with CK, bulk density decreased by 5.6-18.0% while porosity, EC, pH, total N and SOC significantly increased in the organic treatments by 6.0-25.9%, 8.3-25.0%, 0.52-1.7%, 2.7-54.7% and 1.3-18.4% respectively. The textural class of soil under the different treatments did not change however, the distribution of soil particle size varied among the treatments, where high clay and silt content were recorded in the amended fields. Moreover, the application of different organic materials significantly affected the soil aggregate stability and this was attributed to the increase in organic matter content which accelerated important microbial activities in the soil to improve aggregation. At higher suction potentials, higher water contents were recorded in the organic amended fields mainly due to the improved physical properties of the soil. Conclusion: The study results showed that the application of organic amendments greatly improves the physical and chemical properties of black soil. Therefore, using these organic amendments can serve as an effective strategy to enhance soil quality and fertility.

scholarly journals Effects of Soil and Water Conservation Structures on Selected Soil Physicochemical Properties: The Case of Ejersa Lafo District, Central Highlands of Ethiopia

2021 ◽  
Vol 2021 ◽  
pp. 1-11
Author(s):  
Adugna Tolesa ◽  
Siraj Mammo ◽  
Eve Bohnett
Keyword(s):  
Soil Erosion ◽  
Physicochemical Properties ◽  
Soil Properties ◽  
Water Conservation ◽  
Block Design ◽  
Soil Samples ◽  
Soil And Water Conservation ◽  
Soil Physicochemical Properties ◽  
Total N ◽  
Soil And Water

Land degradation in the form of soil erosion and fertility depletion is the major environmental problem in Ethiopia. However, to curb this problem, soil and water conservation (SWC) structures are commonly practiced in many rural parts of Ethiopia. This study was conducted to assess the effects of SWC structures on selected soil physicochemical properties in Ejersa Lafo district. For this study, two kebeles (peasant associations) were selected purposively from the district based on the severity of soil erosion and information on SWC practices. The research design employed in this study was systematic, randomized, complete block design. A total of 12 composite soil samples were collected from the depth of 0 to 20 cm at two subwatersheds, namely, Jamjam laga batu and Koriso Odo guba with SWC and without SWC structures at three landscape positions. All the soil samples were analyzed following the standard and recommended procedures. The effect of independent variables (SWC practices and landscape positions) on the dependent variables (soil properties) was statistically tested using the SPSS computer program 21. In this study, most of the selected soil physicochemical properties were affected by watershed management intervention (SWC) structures. Soil moisture content (SMC), clay, pH, electrical conductivity (EC), total N (TN), available (AP), available K (AK), and organic carbon (OC) were higher in the subwatershed treated with SWC structures (conserved), whereas bulk density, silt, and sand were higher in the subwatershed without SWC structures (nonconserved). Most of the selected soil chemical properties were significantly varied ( p < 0.05 ) between conserved and nonconserved farm land except EC. All the selected soil physicochemical properties did not show any significant variation ( p < 0.05 ) at landscape positions except sandy soil. The physicochemical soil properties of selected parameters were in good conditions in the conserved areas with higher N and OM and lower BD, indicating fertility of the soil compared with the nonconserved land. The implementation of SWC structures improved some of the physicochemical properties of soil, such as SMC, clay particle, pH, EC, total N, AP, AK, and OC in the study area. Furthermore, efforts are required to enhance community adoption towards soil and water conservation. Additionally, further research has to be carried out on socioeconomic aspects and impacts of the intervention on crop productivity for better understanding of the sustainable use of the land.

scholarly journals Evaluation of Physicochemical Properties and Microbial Populations of Soil of Bagale Forest Reserve, Girei Local Government Area, Adamawa State, Nigeria

2020 ◽  
pp. 13-21
Author(s):  
G. O. Ateh ◽  
M. G. Saka ◽  
E. E. Dishan ◽  
B. B. Meer
Keyword(s):  
Local Government ◽  
Physicochemical Properties ◽  
Soil Depth ◽  
Chemical Properties ◽  
Soil Samples ◽  
Local Government Area ◽  
Microbial Populations ◽  
Available Phosphorus ◽  
High Porosity ◽  
Forest Reserve

This study evaluated the relationship between selected physicochemical properties and microbial populations of the soil of Bagale Forest Reserve, Girei Local Government Area of Adamawa State, Nigeria. Five plots of 20 x 20 m were laid. Soil samples were collected from five different positions at two soil depths of 0-15 cm and 15-30 cm. The soil samples were isolated in the laboratory for microbial populations and determination of physical and chemical properties. The results obtained revealed that fungal population (7.65 x 105 cfu/ml) was the highest at the soil depth of 0-15 cm, representing 39% of the total microbial populations in the sampled soil of the study area. The results further revealed that the population (6.84 x 105 cfu/ml) of the bacteria had a positive effect on soils of the study area in terms of nitrogen fixation by Rhizobacterial spp. Chemical properties of the soil samples revealed that the available phosphorus exhibited the highest percentage (61.7%) at 0-15 cm soil depth. Analyses of soil physical properties recorded the highest percentage (49.0%) of sand at 0-15 cm soil depth. A similar percentage (50.0%) of sand was exhibited at the depth of 15-30 cm. These percentages accounted for the high porosity (29.0%) of the soil observed at the two soil levels in the study area and could be improved through the application of lime fertilizers. Application of appropriate fertilizers like NPK to improve the soil condition of the study area is highly recommended.

scholarly journals The effect of invasive species Lantana Camara L. on soil nutrients at Ol-Donyo Sabuk National Park, Kenya

2020 ◽  
Vol 1 (1) ◽  
pp. 25-32
Author(s):  
M N Wekhanya ◽  
P. K. Mbugua ◽  
J. K. Mworia
Keyword(s):  
Soil Nutrients ◽  
National Park ◽  
Soil Samples ◽  
Lantana Camara ◽  
Preventive Strategy ◽  
Native Plant ◽  
Organic C ◽  
Anova Test ◽  
Significant Difference ◽  
Study Sites

The aim of this study was to establish whether the invasive plant Lantana camara L. alters the soil chemical properties at Ol-Donyo Sabuk National Park. The key objective was to evaluate the soil nutrient composition in areas invaded by L. camara and how these differ from areas without L. camara. Five study sites were selected by purposeful sampling, out of the existing 10 blocks. Soil samples were collected randomly from L. camara invaded areas and similarly from adjacent areas free from L. camara. The soil samples were subjected to determination of the following nutrients and parameters: pH, potassium (K), calcium (Ca) magnesium (Mg), total nitrogen (N), phosphorus (P), total organic carbon (TOC), manganese (Mn), copper (Cu), iron (Fe), zinc (Zn) and sodium (Na). The data obtained was analysed using Two-way ANOVA test to determine difference in nutrients composition in L. camara invaded and non-invaded areas. Three-way ANOVA test was used to gauge the interactions between wet and dry season, invaded and non-invaded areas and study sites. A post-ANOVA test, Tukey’s Honest Significant Difference was done to separate the means. The results from the study indicated L. camara invaded areas had a significant difference in pH, P, N, Mn, Fe and total organic C compared to the patches that had native plants and not invaded by L. camara. High pH also makes P to be more available to plants that is why P was high in the L. camara invaded areas. This study revealed that L. camara remarkably changes the concentration and balance of soil nutrients resulting to a change in chemistry of soil nutrients. This is in a bid to suit its survival to the detriment of the native plant species. This study is hence vital for designing an effective eradication and preventive strategy of L. camara in Ol-Donyo Sabuk National Park and other protected ecological habitats in Kenya.

scholarly journals Effects of Land Use, Soil Depth and Topography on Soil Physicochemical Properties along the Toposequence at the Wadla Delanta Massif, Northcentral Highlands of Ethiopia

2016 ◽  
Vol 5 (2) ◽  
pp. 57 ◽  
Author(s):  
Nahusenay Abate ◽  
Kibebew Kibret
Keyword(s):  
Land Use ◽  
Physicochemical Properties ◽  
Soil Depth ◽  
Bottom Layer ◽  
Exchange Capacity ◽  
Available Phosphorus ◽  
Soil Physicochemical Properties ◽  
Cultivated Land ◽  
Topographic Positions ◽  
Effects Of Land Use

The study was conducted to investigate the effects of land use, depth and topography on soil physicochemical properties at the Wadla Delanta Massif, northcentral Ethiopia. Four land uses (natural forest, shrub, grazing and cultivated land), three soil depths (0-20, 20-40, 40-60 cm) and three topographic positions (upper, middle and lower) in three replications were considered for this study. A total of 108 composite samples were collected for laboratory analysis. The results show that particle size distribution was affected by the main effects of land use and soil depth; bulk and particle densities, total porosity, organic matter and total nitrogen contents, C:N ratio and available phosphorus were significantly affected by the interaction of land use by soil depth only, whereas, soil pH, electrical conductivity, exchangeable bases, cation exchange capacity, percent base saturation and extractable micronutrients were affected by the interaction effects of the three factors. Highest clay and bulk density were recorded at the bottom layer of the cultivated land soils, while the utmost porosity, organic matter and nitrogen contents, and available phosphorus were recorded at the surface layers of the natural forest land soils. Highest pH was at the bottom layer of the cultivated land at the three topographic positions. Highest exchangeable bases and cation exchange capacity were observed in the bottom layers of soils under the four land use types at the lower topographic position, whilst extractable micronutrients were recorded at the surface layers of the forest land soils at the upper topographic position. In general, most of the measured soil properties were measured better in forest than in other land use soils and the lower topographic positions than the upper and middle ones. Interaction of land use with topography showed negative effects especially on cultivated and grazing land soils in all topographic positions. Therefore, integrated soil fertility management and soil conservation measures are required in all topographic positions to maintain soil physicochemical properties.

scholarly journals Physicochemical properties of tropical forest top soil in relation to depth in western Nepal

2020 ◽  
Vol 30 (1) ◽  
pp. 39-48
Author(s):  
B. Gautam ◽  
M. K. Chettri
Keyword(s):  
Physicochemical Properties ◽  
Soil Nutrients ◽  
Sustainable Management ◽  
National Park ◽  
Ph Value ◽  
Soil Depth ◽  
Soil Bulk Density ◽  
Resource Extraction ◽  
Available Phosphorus ◽  
Top Soil

Information on soil properties with regards to forest soil-depth are important for sustainable management of forest. The present study investigated the physicochemical properties of the top soil (0−30cm depth) in the three forests, viz. i) the Terai Shorea Forest (Bardia National Park), ii) the Evergreen Riverine Forest (Bardia National Park) and iii) the Puraina CF (Kailali district) of western Nepal. In the tropical forests of western Nepal, the soil texture is, moreover, loamy sand to sand. The soil bulk density ranged from 1.33−1.63 gm cm-3, and slightly increased with the increase in the soil-depth. The soil pH value ranged from 5.77−7.36. The soil organic carbon, total nitrogen (N), available phosphorus (P), and available potassium (K) were found to be in the ranges of 0.54−1.64%, 0.04−0.14%, 4.84−31.72 kg ha-1, and 204.35−557.44 kg ha-1, respectively, and all these values decreased with the increase in the soil-depth in both the forests of the protected area; however, this decreasing trend of the soil nutrients with the increase in the soil-depth was not observed in the Puraina CF as the values of the soil nutrients were lower within 0−10cm in the CF. The soil nutrients with all the depths were found to be the highest in the Terai Shorea Forest. The lower values of the soil nutrients in the Puraina CF were the result of resource extraction.  

scholarly journals High-throughput sequencing analysis of the rhizosphere arbuscular mycorrhizal fungi (AMF) community composition associated with Ferula sinkiangensis

2020 ◽  
Vol 20 (1) ◽  
Author(s):  
Yunfeng Luo ◽  
Zhongke Wang ◽  
Yaling He ◽  
Guifang Li ◽  
Xinhua Lv ◽  
...  
Keyword(s):  
Physicochemical Properties ◽  
Total Phosphorus ◽  
High Throughput ◽  
High Throughput Sequencing ◽  
Nitrate Nitrogen ◽  
Soil Depth ◽  
Slope Position ◽  
Soil Physicochemical Properties ◽  
Ferula Sinkiangensis ◽  
The Relationship

Abstract Background Ferula sinkiangensis is an increasingly endangered medicinal plant. Arbuscular mycorrhiza fungi (AMF) are symbiotic microorganisms that live in the soil wherein they enhance nutrient uptake, stress resistance, and pathogen defense in host plants. While such AMF have the potential to contribute to the cultivation of Ferula sinkiangensis, the composition of AMF communities associated with Ferula sinkiangensis and the relationship between these fungi and other pertinent abiotic factors still remains to be clarified. Results Herein, we collected rhizosphere and surrounding soil samples at a range of depths (0–20, 20–40, and 40–60 cm) and a range of slope positions (bottom, middle, top). These samples were then subjected to analyses of soil physicochemical properties and high-throughput sequencing (Illumina MiSeq). We determined that Glomus and Diversispora species were highly enriched in all samples. We further found that AMF diversity and richness varied significantly as a function of slope position, with this variation primarily being tied to differences in relative Glomus and Diversispora abundance. In contrast, no significant relationship was observed between soil depth and overall AMF composition, although some AMF species were found to be sensitive to soil depth. Many factors significantly affected AMF community composition, including organic matter content, total nitrogen, total potassium, ammonium nitrogen, nitrate nitrogen, available potassium, total dissolvable salt levels, pH, soil water content, and slope position. We further determined that Shannon diversity index values in these communities were positively correlated with total phosphorus, nitrate-nitrogen levels, and pH values (P < 0.05), whereas total phosphorus, total dissolvable salt levels, and pH were positively correlated with Chao1 values (P < 0.05). Conclusion In summary, our data revealed that Glomus and Diversispora are key AMF genera found within Ferula sinkiangensis rhizosphere soil. These fungi are closely associated with specific environmental and soil physicochemical properties, and these soil sample properties also differed significantly as a function of slope position (P < 0.05). Together, our results provide new insights regarding the relationship between AMF species and Ferula sinkiangensis, offering a theoretical basis for further studies of their development.

scholarly journals Soil Nutrient Depletion Is Associated with the Presence of Burkholderia pseudomallei

2016 ◽  
Vol 82 (24) ◽  
pp. 7086-7092 ◽  
Author(s):  
Viriya Hantrakun ◽  
Patpong Rongkard ◽  
Malinee Oyuchua ◽  
Premjit Amornchai ◽  
Cherry Lim ◽  
...  
Keyword(s):  
Organic Matter ◽  
Physicochemical Properties ◽  
Soil Properties ◽  
Soil Nutrients ◽  
Burkholderia Pseudomallei ◽  
Agricultural Practices ◽  
Rice Fields ◽  
Soil Physicochemical Properties ◽  
Content Type ◽  
Calcium Magnesium

ABSTRACTBurkholderia pseudomalleiis a soil-dwelling bacterium and the cause of melioidosis, which kills an estimated 89,000 people per year worldwide. Agricultural workers are at high risk of infection due to repeated exposure to the bacterium. Little is known about the soil physicochemical properties associated with the presence or absence of the organism. Here, we evaluated the soil physicochemical properties and presence ofB. pseudomalleiin 6,100 soil samples collected from 61 rice fields in Thailand. The presence ofB. pseudomalleiwas negatively associated with the proportion of clay, proportion of moisture, level of salinity, percentage of organic matter, presence of cadmium, and nutrient levels (phosphorus, potassium, calcium, magnesium, and iron). The presence ofB. pseudomalleiwas not associated with the level of soil acidity (P= 0.54). In a multivariable logistic regression model, the presence ofB. pseudomalleiwas negatively associated with the percentage of organic matter (odds ratio [OR], 0.06; 95% confidence interval [CI], 0.01 to 0.47;P= 0.007), level of salinity (OR, 0.06; 95% CI, 0.01 to 0.74;P= 0.03), and percentage of soil moisture (OR, 0.81; 95% CI, 0.66 to 1.00;P= 0.05). Our study suggests thatB. pseudomalleithrives in rice fields that are nutrient depleted. Some agricultural practices result in a decline in soil nutrients, which may impact the presence and amount ofB. pseudomalleibacteria in affected areas.IMPORTANCEBurkholderia pseudomalleiis an environmental Gram-negative bacillus and the cause of melioidosis. Humans acquire the disease following skin inoculation, inhalation, or ingestion of the bacterium in the environment. The presence ofB. pseudomalleiin soil defines geographic regions where humans and livestock are at risk of melioidosis, yet little is known about the soil properties associated with the presence of the organism. We evaluated the soil properties and presence ofB. pseudomalleiin 61 rice fields in East, Central, and Northeast Thailand. We demonstrated that the organism was more commonly found in soils with lower levels of organic matter and nutrients, including phosphorus, potassium, calcium, magnesium, and iron. We also demonstrated that crop residue burning after harvest, which can reduce soil nutrients, was not uncommon. Some agricultural practices result in a decline in soil nutrients, which may impact the presence and amount ofB. pseudomalleibacteria in affected areas.

Effects of Ecological Projects on Grassland Soil Physicochemical Properties in Three-River Headwater

2013 ◽  
Vol 807-809 ◽  
pp. 843-847
Author(s):  
Xu Dong Zhao ◽  
De Gang Zhang ◽  
Li Na Shi ◽  
Yong Shun Yang
Keyword(s):  
Organic Matter ◽  
Physicochemical Properties ◽  
Water Content ◽  
Soil Water ◽  
Soil Water Content ◽  
Available Phosphorus ◽  
Soil Physicochemical Properties ◽  
Total N ◽  
Effective Measure ◽  
Artificial Grassland

The depth variations of soil physicochemical properties in the degraded native grasslands and the artificially restored grasslands were studied in the Three-river headwater areas of Qinghai-Tibetan plateau, China. The results showed: (1) With the increase of the gradient of restoration years, soil water content, total chemical properties, total potassium, phosphorus, available phosphorus and potassium were increased thereafter in the artificial grasslands. (2) With the increase of grassland degradation gradient, soil water content was gradually reduced, and the total N, K, the organic matter didnt gradually reduced also. (3) Both restoration years and degradation degree didnt influence the nutrient distribution in soil. (4) The organic matter, total N and K of degraded grassland were increased by artificial grassland construction. Therefore, artificial grassland construction canbe used as an effective measure of ecological projects in the Three-river headwater area.

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