Long-Term Effects of Fertilizers and Manure on Soil and Leaves of Cotton in Nigeria

1969 ◽  
Vol 5 (3) ◽  
pp. 241-247 ◽  
Author(s):  
B. W. Bache ◽  
R. G. Heathcote
Keyword(s):  
Potassium Chloride ◽  
Ammonium Sulphate ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Long Term Effects ◽  
Single Superphosphate ◽  
Exchangeable Ca ◽  
Chemical Properties Of Soils ◽  
Sudan Savanna ◽  
A Site

SummaryOn a site in the Sudan Savanna, chemical properties of soils (except for phosphate) and the composition of cotton leaves were determined after fifteen annual treatments including dung, ammonium sulphate, single superphosphate and potassium chloride, in all combinations of three levels. In the soils dung increased C, N, cation exchange capacity, exchangeable Ca and Mg and pH, and decreased soluble Al and Mn; ammonium sulphate decreased pH, increased soluble Al and Mn, and decreased exchangeable Ca and Mg; potassium chloride had no obvious effects. In the plants dung increased P and reduced Mn; ammonium sulphate reduced Ca and Mg, and increased Mn; superphosphate increased P, Ca and Mg, and reduced K; potassium chloride increased K slightly. The most important results were the ability of ammonium sulphate to acidify the soil, as shown by soil properties and reflected in tissue composition, and the ability of dung to ameliorate these effects. Reduction of crop yield in the presence of adequate nutrient supply seems to have been due to excessive soil acidity.

Soil water repellency persistence after recurrent forest fires on Mount Carmel, Israel

2013 ◽  
Vol 22 (4) ◽  
pp. 515 ◽  
Author(s):  
Naama Tessler ◽  
Lea Wittenberg ◽  
Noam Greenbaum
Keyword(s):  
Organic Matter ◽  
Soil Water ◽  
Forest Fires ◽  
Water Drop ◽  
Chemical Properties ◽  
Water Repellency ◽  
Mediterranean Ecosystem ◽  
Long Term Effects ◽  
Soil Water Repellency ◽  
Chemical Properties Of Soils

Variations in forest fires regime affect: (1) the natural patterns of community structure and vegetation; (2) the physico-chemical properties of soils and consequently (3) runoff, erosion and sediment yield. In recent decades the Mediterranean ecosystem of Mount Carmel, north-western Israel, is subjected to an increasing number of forest fires, thus, the objectives of the study were to evaluate the long-term effects of single and recurrent fires on soil water repellency (WR) and organic matter (OM) content. Water repellency was studied by applying water drop penetration time (WDPT) tests at sites burnt by single-fire, two fires, three fires and unburnt control sites. Water repellency in the burnt sites was significantly lower than in the unburnt control sites, and the soil maintained its wettability for more than 2 decades, whereas after recurrent fires, the rehabilitation was more complicated and protracted. The OM content was significantly lower after recurrent than after a single fire, causing a clear proportional decrease in WR. The rehabilitation of WR to natural values is highly dependent on restoration of organic matter and revegetation. Recurrent fires may cause a delay in recovery and reduced productivity of the soil for a long period.

Organic C and nutrients in surface soils from some primary rainforests, derived grasslands and secondary rainforests on the Atherton Tableland in North East Queensland

Soil Research ◽  
1993 ◽  
Vol 31 (3) ◽  
pp. 343 ◽  
Author(s):  
J Maggs ◽  
B Hewett
Keyword(s):  
Metamorphic Rock ◽  
Forest Type ◽  
Mineral Soil ◽  
Chemical Properties ◽  
Primary Forest ◽  
Long Term Effects ◽  
Organic C ◽  
North East ◽  
Exchangeable Ca ◽  
Labile N

Some long term effects of (a) converting rainforest to grassland, and (b) rainforest regeneration on cleared land were investigated by comparing chemical properties of mineral soil (0-10 cm depth) from beneath primary rainforest, derived grassland and old secondary rainforest. Grasslands and secondary rainforest. were on land cleared at least 50 years ago. The study was undertaken on the Atherton Tableland in north east Queensland using soils formed on basalt, granite and metamorphic rocks. Organic C, kjeldahl N and labile N were 15-50% lower (P < 0.05) beneath grassland than primary rainforest for all soils, and were higher beneath secondary rainforest than grassland. Exchangeable Ca varied in a similar way in basaltic soils but did not differ between vegetation types in the other soils. Extractable Al was lower under grassland than either forest type for soils formed on granite and metamorphic rock. Total and organic P concentrations did not differ between primary forest and grassland, but were lowest under secondary rainforest for soils on metamorphic rock.

LONG-TERM EFFECTS OF LIME ADDITIONS ON SUGARCANE YIELD AND SOIL CHEMICAL PROPERTIES IN NORTH QUEENSLAND

2000 ◽  
Vol 36 (3) ◽  
pp. 397-413 ◽  
Author(s):  
A. D. NOBLE ◽  
A. P. HURNEY
Keyword(s):  
Acid Soil ◽  
Ion Pairs ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Cane Yield ◽  
Long Term Effects ◽  
Exchangeable Acidity ◽  
Long Term Study ◽  
Highly Weathered Soils

In many highly weathered soils of the humid tropics, crop exploitation of the subsoil environment is limited through acid soil infertility. Since the use of mechanical profile modification is often prohibitive, surface incorporation of soil amendments is often the only means available to rectify this problem. A field trial was established with sugarcane on a strongly Acidic Dystrophic Brown Dermosol (Oxic Humitropept) in 1978 to evaluate the effects of surface incorporated lime additions on yield and performance of sugarcane. Eighteen years after the establishment of this trial, significant responses in cane yield were still evident following a single application of 5 t lime ha−1 made in 1978, as well as repeated applications of 5 t ha−1 on three occasions over the past 18 years. Progressive reductions in exchangeable acidity were accompanied by increases in subsoil Ca2+ and Mg2+. Soil pH increased significantly to a depth of 100 cm, this being attributed to the formation of ion pairs with NO3 in the surface soil, the subsequent leaching of these complexes and the differential uptake of NO3 at depth by roots. The results from this long-term study indicate that surface incorporation of lime is an economically viable approach to the remediation of subsoil acidity on soils such as those studied, namely, those with a low inherent cation exchange capacity and anion exchange capacity.

Properties of soils in the marginal upland of Sta. Rita, Samar, Philippines

2017 ◽  
pp. 1-19
Author(s):  
Kenneth Oraiz ◽  
Victor Asio
Keyword(s):  
Crop Production ◽  
Chemical Properties ◽  
The Philippines ◽  
Exchange Capacity ◽  
Ecological Problem ◽  
High Porosity ◽  
Total N ◽  
Upland Soils ◽  
Chemical Properties Of Soils ◽  
High Base

The widespread occurrence of marginal uplands is a serious agricultural and ecological problem in the Philippines. The study evaluated the morphological and physico-chemical properties of soils in the marginal upland of Sta. Rita, Samar. Three soil profiles located at different physiographic positions were examined and sampled. Findings revealed that the marginal upland soils were derived from mudstone. They were characterized by an Ap-Bt-BC horizon sequence and they were clayey with moderate to high porosity and water holding capacity values. The soils were friable in their surface horizons when moist, but plastic and sticky when wet. The soils had pH(water) values ranging from 5.20 to 6.86, indicating that soil acidity was not yet a serious problem in these soils. The soils had moderate soil organic matter contents in their surface horizons but low amounts in subsurface horizons. Total N and available P of the soils were low and a problem for crop production. However, the soils had moderate to high exchangeable bases and cation exchange capacity values. In terms of degree of soil development, the marginal upland soils was observed to be mature as reflected by their horizonation, particularly by the presence of an argillic horizon (B horizon with high clay accumulation). But they still had high base saturation, suggesting that they were not yet highly leached and thus, were classified as Typic Hapludalfs or Haplic Luvisols.

Spatial distribution of basic exchangeable cations under different land uses in soils of Hamelmalo, Eritrea

2017 ◽  
Vol 2 (02) ◽  
pp. 152-157
Author(s):  
Huma Naz ◽  
Million Weldetensae ◽  
B. B. Kanwar ◽  
Balwan Singh
Keyword(s):  
Sandy Loam ◽  
Chemical Properties ◽  
Clay Content ◽  
Exchangeable Cations ◽  
Land Uses ◽  
Surface Samples ◽  
Agricultural College ◽  
Exchangeable Ca ◽  
The Status ◽  
Chemical Properties Of Soils

The study was conducted at two sites; Hamelmalo Agricultural College and Basheri watershed area in sub Zoba Hamelmalo, Keren to determine the status of basic exchangeable cations (Ca, Mg, K and Na) under different land uses and their relationship with physco-chemical properties of soils. Global Positioning System based soil samples were collected randomly from different land use systems, cultivated (cereals and horticulture) and non-cultivated open wood lands. The pH values ranged from neutral to strongly alkaline and electrical conductivity values were found to be non-saline in nature. The textures of majority of the surface samples were found sandy loam. Availability of exchangeable Ca++, Mg++, K+ and Na+ in surface soils of all land uses varied from high to very high, moderate to high, very low to low and very low to moderate, respectively. Exchangeable K+ showed highly significant positive correlation (p less than 0.01) with clay content. However exchangeable Ca++ contents in soil was positively and significantly correlated (p less than 0.05) with pH, clay, silt and negative significant correlation (p less than 0.05) with BD. Mg++ had positive significant correlation (p less than 0.05) with clay content and negative significant correlation (p less than 0.05) with sand.

scholarly journals Chemical properties of soils treated with biological sludge from gelatin industry

2012 ◽  
Vol 36 (2) ◽  
pp. 653-660 ◽  
Author(s):  
Rita de Cássia Melo Guimarães ◽  
Mara Cristina Pessôa da Cruz ◽  
Manoel Evaristo Ferreira ◽  
Carlos Alberto Kenji Taniguchi
Keyword(s):  
Organic Matter Content ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Matter Content ◽  
P Availability ◽  
Base Content ◽  
Biological Sludge ◽  
Randomized Design ◽  
Chemical Properties Of Soils ◽  
The Impact

The impact of agro-industrial organic wastes in the environment can be reduced when used in agriculture. From the standpoint of soil fertility, residue applications can increase the organic matter content and provide nutrients for plants. This study evaluated the effect of biological sludge from gelatin industry on the chemical properties of two Ultisols (loamy sand and sandy clay) and an Oxisol (clay). The experiment lasted 120 days and was carried out in laboratory in a completely randomized design with factorial arrangement, combining the three soils and six biological sludge rates (0, 100, 200, 300, 400, and 500 m³ ha-1), with three replications. Biological sludge rates of up to 500 m³ ha-1 decreased soil acidity and increased the effective cation exchange capacity (CEC) and N, Ca, Mg, and P availability, without exceeding the tolerance limit for Na. The increase in exchangeable base content, greater than the effective CEC, indicates that the major part of cations added by the sludge remains in solution and can be lost by leaching.

NUTRIENT VARIABILITY OF FOREST FLOORS NEAR PORT HARDY, BRITISH COLUMBIA, CANADA

1980 ◽  
Vol 60 (3) ◽  
pp. 565-573 ◽  
Author(s):  
H. J. QUESNEL ◽  
L. M. LAVKULICH
Keyword(s):  
Forest Floor ◽  
Chemical Properties ◽  
Sampling Procedure ◽  
Exchange Capacity ◽  
Forest Sites ◽  
Exchangeable Ca ◽  
Allowable Error ◽  
Forest Floors ◽  
Nutrient Variability ◽  
Physical And Chemical

The variability of forest floor properties over short distances and the number of samples required to achieve desired levels of precision for estimation of property means have received little attention. The importance of the forest floor for forest management is well known and increasingly forest floor characteristics are being used to classify forest sites. Highly variable forest floor properties require more intensive sampling and often have less predictive value for characterization and classification purposes. A study site at Port Hardy was used to characterize forest floors for selected physical and chemical properties. The three sites chosen represented xeric, mesic and hygric positions along a hygrotopic gradient. A stratified random sampling procedure was used to obtain 15 samples at each site. Fifteen samples were adequate to characterize the means at 10% allowable error with a 95% confidence level for total nitrogen, organic carbon, pH and cation exchange capacity. Greater than 15 samples were required for exchangeable bases and forest floor thickness for the same level of accuracy and confidence. Even at 25% allowable error and 90% confidence, 40 samples and 16 samples, respectively, were required for exchangeable Ca and Mg.

Altered forest composition and soil properties of historic charcoal hearths in southeastern Pennsylvania

1995 ◽  
Vol 25 (5) ◽  
pp. 687-696 ◽  
Author(s):  
Carl J. Mikan ◽  
Marc D. Abrams
Keyword(s):  
Chemical Properties ◽  
Basal Area ◽  
Exchange Capacity ◽  
Forest Composition ◽  
Charcoal Production ◽  
Exchangeable Ca ◽  
Quercus Species ◽  
Stump Sprouting ◽  
Physical And Chemical ◽  
Charcoal Hearths

This study related age structure and composition of forests in southeastern Pennsylvania to edaphic properties caused by the activities of a local charcoal iron furnace from the late 18th to the late 19th century. Forests surrounding charcoal hearths were harvested on 20- to 30-year rotations to supply wood for charcoal production in earthmound kilns. Charcoal hearths were created by a recurring cycle of disturbance, including the removal of established vegetation, intense heat, and the deposition of charcoal. Thirty-eight hearths of Hopewell Furnace National Historic Site were examined to describe differences in vegetation relative to surrounding forests that have developed since the cessation of charcoal production in 1883. Hearth forests were significantly younger than surrounding forests, with lower tree density and basal area, decreased sapling and shrub abundance, and higher herbaceous cover. Compositional differences on charcoal hearths included decreased importance of several Quercus species and ericaceous shrubs and increased importance of Liriodendrontulipifera L. Results of this study indicated that the initial effect of charcoal production was the prevention of stump sprouting and a delay in recolonization following disturbance due to extreme soil physical and chemical properties. Failure of hearth seedlings to recruit into larger size classes, age–diameter relationships of Liriodendrontulipifera L. trees, and the failure of calcifuge species to reestablish similar cover on charcoal hearths suggested that unfavorable properties of charcoal soils continue to negatively affect long-term productivity. Relative to nonhearth soils, large, significant differences in soil pH, cation exchange capacity, base saturation, and exchangeable Ca, Mg, and K indicated that continuing inhibition of woody plants on charcoal hearths may be related to alterations in soil chemistry that have persisted for 110 years.

scholarly journals Effects of Management Practices on Soil Properties and Plant Nutrition in Hay Meadows in Picos de Europa

Environments ◽  
2021 ◽  
Vol 8 (5) ◽  
pp. 38
Author(s):  
Judith Álvarez ◽  
Elías Afif ◽  
Tomás E. Díaz ◽  
Laura García ◽  
Jose A. Oliveira
Keyword(s):  
Soil Properties ◽  
Management Practices ◽  
Chemical Properties ◽  
Clay Content ◽  
Exchange Capacity ◽  
Nutrient Concentrations ◽  
Mean Values ◽  
Hay Meadows ◽  
Natural Grasslands ◽  
Chemical Properties Of Soils

Fertilization and mowing affects the physico-chemical properties of soils, as well as the characteristics of the plants growing on them. Changes in the management techniques are causing semi-natural grasslands to disappear all over Europe. These grasslands host a great amount of diversity, thus their conservation is a top priority. This work studies whether the kind of management has an influence on the soil properties and the foliar content in macronutrients in 25 hay meadows located in Picos de Europa (10 in Asturias, 10 in Castilla y León and 5 in Cantabria). Soils at a 0–20 cm depth showed a high content of organic matter and a low C/N ratio. Effective cation exchange capacity was adequate for a texture, which varied from sandy clay loam to loam, with an average clay content of 17%. Mean values of foliar nutrient concentrations showed a deficiency in K. In this study, management practices were shown to affect some properties of the soils, namely pH, sand percentage and exchangeable K and Ca, to different extents. The highest values of pH and exchangeable Ca were significantly correlated with the least intensive management.

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