scholarly journals Evaluation of Primary Macro Nutrients on Arboretum Area in Lampung University Campus, Gedong Meneng

2015 ◽  
Vol 19 (2) ◽  
pp. 91
Author(s):  
Nur Afni Afrianti ◽  
Tamaluddin Syam
Keyword(s):  
Organic Matter ◽  
Soil Fertility ◽  
Cover Crop ◽  
Soil Characteristics ◽  
Survey Method ◽  
University Campus ◽  
Organic C ◽  
Tree Litter ◽  
Physical And Chemical ◽  
Macro Nutrients

Vegetation has a strong influence on soil characteristics. Vegetation can contribute organic matter sand nutrients to the soil. This study aimed to assess soil fertility through various approaches physical and chemical soil on various types of cover crop in the  arboretum area at University of Lampung, and determined the type of cover crop that had the best effect on soil fertility. The research was be conducted by a survey method, which made observations on the soil characteristics of six species of cover crops following were rosewood (Dalbergia latifolia), teak (Tectona grandis), albizia (Paraserianthes Albiziaria), acacia (Acasia mangium), fern tree (Filicium desipiens), and mahogany (Swietenia macrophylla King). Soil characteristics observed data were the physical and chemical properties, obtained by field observations, through boring profiles and soil sampling. The results showed that soil fertility on rosewood, albizia, acacia and mahogany on campus area of Lampung University had contents of soil organic C, organic matter, and soil total N higher than teak and Fern tree. Litter from Rosewood, Albizia, and acacia had the best effect on soil fertility, so they could be the best covered vegetation to improve soil characteristics related to optimal and sustainable of land management.Keyword : Acacia, albizia, arboretum, cover crop, fern tree, litter, macronutrient, mahogany, rosewood, teak, and vegetation. [How to Cite: Nur AA and T Syam. 2014. Evaluation of Primary Macro Nutrients on Arboretum Area in Lampung University Campus, Gedong Meneng. J Trop Soils 19(2): 101-107. Doi: 10.5400/jts.2014.19.2.101]   

scholarly journals Karaktersitik Lahan Agroforestri

2017 ◽  
Vol 4 (1) ◽  
pp. 1-6
Author(s):  
Fahruni Fahruni
Keyword(s):  
Land Use ◽  
Soil Fertility ◽  
Hevea Brasiliensis ◽  
Soil Analysis ◽  
Nutrient Content ◽  
Soil Characteristics ◽  
Organic C ◽  
Before And After ◽  
The Moment ◽  
Macro Nutrients

Soil quality can be maintained through wise land use. Agroforestry is a solution for land use that keeps soil fertility at the moment. Land use through this agroforestry combines forestry crops with agriculture and/or livestock on a rotating or alternating land. The purpose of this research is to know soil characteristics in rubber agroforestry pattern (Hevea brasiliensis Muell, Arg.). As an interrupted plant Arachis hypogeae. This study was conducted with soil analysis before and after intercropping. Comparing the composition and value of macro nutrient content. Soil characteristics after agroforestry exploitation can be seen from the improvement of macro nutrients, namely: N elements increased from 0.16 mg/100gr to 0.45 mg/100gr. Element P increased from 5.57 to 8.93. For element K of 15.87 increased to 41.50 and organic C increased from 0.83 to 1.55.

scholarly journals ANALISIS TANAH UNTUK REKOMENDASI PEMUPUKAN PADA BUDIDAYA JAGUNG, PADI DAN KETELA POHON

2015 ◽  
Vol 30 (2) ◽  
pp. 91
Author(s):  
Bagus Sri Mulyanto ◽  
Supriyadi Supriyadi ◽  
Djoko Purnomo
Keyword(s):  
Organic Matter ◽  
Plant Growth ◽  
Soil Fertility ◽  
Survey Method ◽  
High Dose ◽  
Nutrient Elements ◽  
Fertility Status ◽  
Chemical Content ◽  
Soil Fertility Status ◽  
Macro Nutrients

<p><em>The application of fertilization and giving organic matter of different causes differences in soil fertility status, with the availability of macro nutrients on a farm, then to know the action proper fertilization. The purpose of this study is to determine the dose fertilization fertility status of the local potential. The research was conducted using a survey method, ie by observing and sampling the soil directly in the field, followed by laboratory analysis to determine the chemical content of the soil. The results showed the level of soil fertility in Wonogiri low fertilizer needs are different in each district in Wonogiri. Areas with low nutrient availability will provide a high dose of fertilizer, and conversely a low fertilization results indicate the availability of nutrient elements in the soil are sufficient for plant growth, although it should still be nurtured to backup next season.</em></p>

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 Soil Fertility Assessment of Semiarid Soils from Nigeria Cropped to Sorghum

2020 ◽  
pp. 36-46
Author(s):  
Nasiru M. Danmowa ◽  
Peter Nkedi- Kizza ◽  
Kelly T. Morgan ◽  
Kamal Mahmoud
Keyword(s):  
Organic Matter ◽  
Soil Fertility ◽  
Ammonium Acetate ◽  
Extraction Methods ◽  
Soil Samples ◽  
Available P ◽  
Northern Nigeria ◽  
Semiarid Soils ◽  
Sorghum Production ◽  
Macro Nutrients

The aim of this study is to characterize the fertility status of the Dingyadi soils from semiarid Northern Nigeria, by using different methods of extraction to assess the potential for soil available macro and micronutrients to the sorghum crop. The study also compared concentrations of extractable nutrients between extractants for ascertaining the possibility of using one method to quantify a variety of plant-available nutrients in soils. Surface (0-15 cm) and sub-surface (15-30 cm) soil samples were collected along a topo-sequence at Dingyadi Sokoto-Nigeria, where sorghum had been grown, to characterize the soil chemical and physical properties that can influence soil fertility for sorghum production. The topo-sequence consisted of valley floor (TLL1), middle (TUP2), and crest (TUP3) positions of the slope. At each position 60 concentrations of each plant nutrient were used for the comparisons.Soil extraction for nutrients was carried out at the Environmental Soil Physics laboratory, Soil and Water Sciences Department, University of Florida, while analysis of aliquots for the elements was carried out at the Southwest Florida Research and Education Center, Immokalee, Florida. The study was carried out over a period of eight months, in 2016-2017. Soil samples were extracted using different extraction methods (Mehlich-3, Bray-1, Ammonium acetate, and DI-Water). A soil to solution ratio of 1:1 was used across all extraction methods to facilitate comparison between methods. However, a test was carried out to examine the effect of soil to solution ratio of (1:10) on extractable macro nutrients using Mehlich3 for randomly selected soil samples across the topo-sequence. Soil samples were also analyzed for texture, pH, organic matter, and cation exchange capacity (CEC). All soil soils were sandy, low in organic matter content, and CEC.With respect to sorghum production, the soils had adequate nutrients (Mg, Ca, K, and P) and soil pH. All soil samples contained no exchangeable K. Mehlich3 extracted higher available P than Bray1 in TLL1, but equal amounts in TUP2 and TUP3. Good correlations exist between extracting methods for macro nutrients (Mg, Ca, K, and P). Bray1 method used for available P is not suitable for soils that have pH greater than 7 determined in water. Mehlich3 is more suitable for the semiarid soils of Northern Nigeria that are acidic or alkaline. The Mehlich3 method should be calibrated with yield response of crops to substitute for Bray1 available phosphorus. Also, Mehlich3 method could be used for the multi-nutrient test with a good correlation with other methods like ammonium acetate for exchangeable bases.

Effects of mineral and organic fertilizers on soil organic carbon fractions in agricultural chestnut soil

2018 ◽  
Vol 22 (03) ◽  
pp. 103-108
Author(s):  
Enkhtuya D ◽  
Tuul D ◽  
Munkhtsetseg T
Keyword(s):  
Land Use ◽  
Organic Matter ◽  
Organic Carbon ◽  
Soil Organic Carbon ◽  
Soil Fertility ◽  
Active Form ◽  
Chestnut Soil ◽  
Organic Fertilizers ◽  
Stable Form ◽  
Organic C

Soil organic matter can be analyzed on the basis of the different fractions. Changes in the levels of organic matter, caused by land use, can be better understood by alterations in the different fractions. Therefore in order to discover tendency of soil fertility sustainability it is significant to research on stable and labile form fractions of soil organic carbon by advanced methodology and modern technique. Our research work aimedto evaluate the effect of mineral and organic fertilizers on the labile and stable organic carbon of the chestnut soil in Mongolia. The soils samples used in this study we collected from variants of mineral (N60P40K40), organic (biohumus 1t / hec.) Fertilizer and their combination of the Long-term fertilizers experiments of Plant and Agriculture Institute Changes in soil organic C by land use for agricultural purposes occurred mainly in the fraction of particulate organic matter (> 20 μm). The clay and silt fractions were quatified with a Mastersizer S after distruction organic substances and carbonates using H2O2 and HCI and the sand fraction was determined by wet sieving. According to our research, the stable form of organic carbon in chestnut soil is 39, 0-40,1% of the total fine particle size and 59, 9-61,0% of the active form fraction. On the other hand, variants with fertilizer tend to have increased stabile composition of soil organic carbon. It indicates that soil fertility protection and increased stability are possible in the country’s agricultural technology if use mineral and organic fertilizers.

scholarly journals Changes of soil agrichemical characteristics in pastures influenced by mineral fertilizing

2011 ◽  
Vol 59 (1) ◽  
pp. 113-120 ◽  
Author(s):  
Stanislav Hejduk
Keyword(s):  
Organic Matter ◽  
Soil Organic Matter ◽  
Ph Value ◽  
Nutrient Content ◽  
Soil Characteristics ◽  
Period Range ◽  
Organic C ◽  
Available Nutrients ◽  
K Concentration ◽  
Forage Yields

Grasslands fertilizing is used for increasing of forage yields and quality and simultaneously for soil fertility maintenance. The aim of this study was to evaluate the effect of mineral fertilizing on basic agrichemical soil characteristics (pH, available nutrients) and soil organic matter at grazing exploitation of grasslands. 60 kg N.ha−1 was applied in the year of experiment establishment and 90 kg N, 30 kg P a 90 kg K ha−1 in each of following four years. Significantly higher pH (+0.17), available P (+48.5%), K (+15.4%) and organic C (+8.8%) content was found at fertilized treatment. pH value varied significantly during experiment period (range 0.6) and correlated inversely with proportion of white clover in first cut (r = −0.499). Although available K in soil was only on satisfactory level (less than good), K concentration in the forage was even from unfertilized plots higher than physiological requirement of plants. Available nutrient content constitutes only small proportion of total nutrient content: 5.1% at P, 2.1% at K, 12.0% at Mg and 39.0% at Ca.

scholarly journals Dampak Kebakaran Hutan Terhadap Flora Dan Sifat Tanah Mineral Di Kawasan Hutan Kabupaten Pelalawan Provinsi Riau

2019 ◽  
Vol 10 (1) ◽  
pp. 40-44
Author(s):  
Basuki Wasis ◽  
Bambang Hero Saharjo ◽  
Robi Deslia Waldi
Keyword(s):  
Organic Matter ◽  
Soil Respiration ◽  
Soil Fertility ◽  
Forest Fires ◽  
Forest Biomass ◽  
Soil Samples ◽  
Organic C ◽  
Mineral Soils ◽  
Total Fungi ◽  
Research Show

Forest fires cause the death of flora, soil damage and smoke disasters. The research was corected at the productivity forest and soil samples were taken through purposive sampling. The result of research show that forest fires cause the death of flora by 100% and erosion occurring at the dept of 5-10 cm. Forest fires cause a significant increase in pH, Ca and Mg mineral soils, and reduce organic C, total microorganisms, total fungi and soil respiration significantly. Forest fires increase soil pH and soil fertility due to ash remaining combustion. The residual combustion ash comes from organic material (natural forest biomass and organic matter) which is burned was which of nutrient needed fan the growth of the vegetation in the forest.Keywords: forest fires, mineral soils, soil fertility, soil properties

scholarly journals Earthworm Abundance and Soil Characteristics Following Cocoa Waste and Manure Applications

2020 ◽  
Vol 36 (1) ◽  
Author(s):  
Erwin Prastowo ◽  
Lina Dwi Agustina ◽  
Cahyo Prayogo
Keyword(s):  
Soil Moisture ◽  
Soil Fertility ◽  
Soil Characteristics ◽  
Field Investigation ◽  
Organic Wastes ◽  
Fertility Level ◽  
Total N ◽  
Organic C ◽  
Top Soil ◽  
Earthworm Population

Soil fertility level improvement in an environmentally friendlier way has been a key to provide a sustainable cocoa production. Earthworms, as decomposeragents in soil, may provide a sustainable way of improving soil fertility level. The objective of this study was to quantify top soil earthworm population andsome important soil characteristics, e.g. soil moisture, organic C, total N, and pH to see if there was any response observed due to different level and type oforganic waste applications. Their surface populations, i.e. at 5–10 cm depth, within cocoa circle were investigated with respect to different type of organic wasteapplications, i.e. cocoa pod waste, cocoa leaf waste, and sheep manure. For cocoa derived organic matter, the level of application was arranged at 5, 10, and 20 ton/ha to obtain an optimal condition at which the highest population of earthworm is obtained. A field investigation was performed at a square of 900 cm2 sizedarea, and extending down to 5–10 cm depth. Additionally, the effect of organic waste to top soil characteristics were also determined mainly to some importantparameters such as soil moisture, organic carbon, total nitrogen, and soil pH (H2O). Our analysis suggest that field heterogeneity condition may limit the conclusion, mainly related to the question of to what extent the effect of organic wastes to the changes in terms of soil characteristics. The application of organic wastes was able to increase the population of earthworms. Their highest abundance was obtained following the application of cocoa pod at 20 ton/ha, which was about 5 times higher than the population in the control. 

The role of active fractions of soil organic matter in physical and chemical fertility of Ferrosols

Soil Research ◽  
1998 ◽  
Vol 36 (5) ◽  
pp. 809 ◽  
Author(s):  
M. J. Bell ◽  
P. W. Moody ◽  
R. D. Connolly ◽  
B. J. Bridge
Keyword(s):  
Organic Matter ◽  
Soil Organic Matter ◽  
Management Practices ◽  
Chemical Properties ◽  
Aggregate Stability ◽  
Infiltration Rate ◽  
Exchange Capacity ◽  
Organic C ◽  
Wide Range ◽  
Physical And Chemical

The relationships between fractions of soil organic carbon (C) oxidised by varying strengths of potassium permanganate (KMnO4) and important soil physical and chemical properties were investigated for Queensland Ferrosols. These soils spanned a wide range of clay contents (31-83%), pH values (4·4-7·9; 1 : 5 water), and total C contents (12· 1-111 g/kg). Carbon fractions were derived by oxidation with 33 mM (C1), 167 mM (C2), and 333 mM (C3) KMnO4, while organic C and total C were determined by Heanes wet oxidation and combustion, respectively. Aggregate stability was determined by wet sieving soil from the surface crust after 30 min of high intensity (100 mm/h), simulated rainfall on disturbed samples in the laboratory. The proportion of aggregates <0·125 mm (P125) was used as the stability indicator because of the high correlation between this size class and the final rainfall infiltration rate (r2 = 0qa86, n = 42). The soil organic C fraction most closely correlated with P125 was C1 (r2 = 0·79, n = 42). This fraction was also highly correlated with final, steady-state infiltration rates in field situations where there were no subsurface constraints to infiltration (r2 = 0·74, n = 30). Multiple linear regression techniques were used to identify the soil properties determining effective cation exchange capacity (ECEC, n = 89). Most variation in ECEC (R2 = 0 ·72) was accounted for by a combination of C1 (P < 0·0001) and pH (P < 0·0001). These results confirm the very important role played by the most labile (easily oxidised) fraction of soil organic matter (C1) in key components of the chemical and physical fertility of Ferrosols. Management practices which maintain adequate C1 concentrations are essential for sustainable cropping on these soils.

Sign in / Sign up

Export Citation Format

Share Document