THE INFLUENCE OF BASE SATURATION AND FERTILITY TREATMENTS ON YIELD AND CATION COMPOSITION OF CROPS GROWN ON TWO BRITISH COLUMBIA SOILS HIGH IN ORGANIC MATTER

1961 ◽  
Vol 41 (1) ◽  
pp. 52-67 ◽  
Author(s):  
J. D. Beaton ◽  
Neville A. Gough ◽  
C. A. Rowles
Keyword(s):  
British Columbia ◽  
Organic Matter ◽  
Calcium Uptake ◽  
Calcium Absorption ◽  
Organic Soil ◽  
Magnesium Content ◽  
Base Saturation ◽  
Cation Composition ◽  
Fertility Treatments ◽  
Soil Calcium

The influence of base saturation and fertility treatments on yield and cation composition of oats grown on two British Columbia soils high in organic matter was studied in the greenhouse. Increased base saturation significantly increased: the yield of oat forage on the Alouette soil (an organic soil), calcium uptake on both soils, magnesium content of oats grown on the Pitt soil, and tissue potassium with the Alouette soil.The yield decreased significantly when nitrogen was added to the Alouette soil. Nitrogen significantly increased tissue calcium on the Pitt soil. The magnesium and potassium content of oats was not influenced by nitrogen.With the Pitt soil there was a consistent (but not significant) trend showing that phosphorus increased yields. For the Alouette soil the interaction between phosphorus and base saturation significantly increased calcium absorption. Phosphorus tended to increase calcium uptake from both soils. Tissue magnesium increased significantly when phosphorus was added to the Pitt soil.There was a tendency (not significant) with both soils for yield to decrease as potassium was applied. When potassium was added to the Pitt soil there was a marked tendency for tissue magnesium to increase. A reverse trend occurred with the Alouette soil. Potassium fertilization of both soils significantly increased potassium absorption.

Response of lodgepole pine health to soil disturbance treatments in British Columbia, Canada

2015 ◽  
Vol 45 (8) ◽  
pp. 1045-1055 ◽  
Author(s):  
Anya M. Reid ◽  
William K. Chapman ◽  
John Marty Kranabetter ◽  
Cindy E. Prescott
Keyword(s):  
British Columbia ◽  
Organic Matter ◽  
Soil Compaction ◽  
Lodgepole Pine ◽  
Mineral Soil ◽  
Forest Health ◽  
Soil Disturbance ◽  
Base Saturation ◽  
Soil Productivity ◽  
Health Response

Soil disturbance from organic matter loss and soil compaction can impair site productivity, but less is known about whether these disturbances also affect forest health (defined here as the presence and severity of damaging pests and diseases, mortality, and overall vigour). We used six long-term soil productivity (LTSP) sites in the interior of British Columbia, Canada to test the effects of organic-matter removal and soil compaction on forest health, and to explore the relationship between forest health response and potential indicators of site sensitivity: mineral soil pH, base saturation, carbon to nitrogen ratio (C:N), carbon to phosphorus ratio (C:P), and calcium to aluminum ratio (Ca:Al). Visual forest health surveys were conducted on 5400 15 and 20 year old lodgepole pine (Pinus contorta Dougl. ex Loud.) trees. Soil disturbance treatments significantly affected forest health metrics, but this response typically differed among sites. Principle component analyses indicated the response of healthy trees was negatively related to soil base saturation, the response of dead or dying trees related to soil C:P, and the response of tree disease related to soil Ca:Al, pH, base saturation, and C:N. We found forest health response to soil disturbance varied among sites with relationships between response and soil chemical properties, suggesting a greater vulnerability of pine stands to disease with increasing soil acidity.

SOIL PROPERTIES AFFECTING THE RETENTION OF PHOSPHORUS FROM EFFLUENT

1971 ◽  
Vol 51 (3) ◽  
pp. 315-322 ◽  
Author(s):  
MATT K. JOHN
Keyword(s):  
Waste Water ◽  
British Columbia ◽  
Organic Matter ◽  
New Zealand ◽  
Soil Properties ◽  
Base Saturation ◽  
Factors Affecting ◽  
Coastal Soils

Factors affecting removal of P from waste water effluent on 376 soils from British Columbia and six soils from New Zealand were studied. When shaken at a ratio of 1:50 soil to effluent, the soils of the dry British Columbia interior removed on an average 31% of the effluent P, whereas wet coastal soils removed 85% and the New Zealand soils removed 76%. The capacity of the soil to remove effluent P was related mostly to Al, Fe and P extracted by various extractants, pH, base saturation, organic matter and texture.

EFFECTS OF INTENSIVE VEGETABLE PRODUCTION ON CHEMICAL PROPERTIES AND NUTRIENT MINERALIZATION OF A BRITISH COLUMBIA HUMISOL

1990 ◽  
Vol 70 (3) ◽  
pp. 445-460
Author(s):  
B. M. OLSON ◽  
L. E. LOWE
Keyword(s):  
British Columbia ◽  
Organic Matter ◽  
Surface Layer ◽  
Subsurface Layer ◽  
Chemical Properties ◽  
Organic Soil ◽  
Yield Reduction ◽  
Main Concern ◽  
Vegetable Production ◽  
Nutrient Mineralization

A study was conducted to determine the effects of long-term vegetable production on some organic matter (OM) chemical properties in an organic soil located near Cloverdale, British Columbia. Producers in this area are concerned about yield reduction and some feel this is due to changes in the soil quality. Paired soil samples were collected from two transects: one in a 40-yr-old vegetable field, and the other in an adjacent fence row. The transects were positioned in order to collect samples from a relatively deep organic deposit and from a shallow deposit where a ridge of mineral subsoil had been exposed. Initial analysis showed that cultivation had changed some chemical properties only in the plow layer. The exception was pH which was higher throughout the sample depth of the cultivated transect. Organic matter loss from the cultivated field was estimated 28% by weight, based on ash accumulation. In the cultivated deep organic section (west of the ridge) OM and C contents were reduced by 7.1 and 5.6% respectively, whereas on the cultivated ridge OM, C, N and S contents and the amount of C, N and S mineralized were reduced by 43.3, 41.6, 43.4, 25.9, 42.8, 60.8 and 52.5%, respectively. On an ash-free basis there were no changes in the deep organic section. In the ridge, the OM sulphur content had increased and the amount of N and S mineralized were decreased compared with the uncultivated transect. In the cultivated surface layer, increased S content in the OM was caused by incorporation of a S-rich subsurface layer during tillage operations. Increases in P content in the cultivated transect were attributed to P fertilization. Within the cultivated transect, C, N and S contents in the exposed mineral ridge were 48, 48, and 44%, respectively, lower than in the deep organic surface layer on the west side of the ridge. The C:N ratios were unchanged at about 16. The chemical stability of the OM was attributed to its well-decomposed nature. At this particular site, the degradation due to excessive cultivation was manifested mainly in OM loss, rather than in changes in OM quality. The main concern of producers is to reduce or prevent further loss of soil OM. Key words: Humisol, organic soil, cultivation, mineralizable C, N and S, incubation

Studying Organic Matter Molecular Assemblage within a Whole Organic Soil by Nuclear Magnetic Resonance

2008 ◽  
Vol 37 (4) ◽  
pp. 1501-1509 ◽  
Author(s):  
Charisma Lattao ◽  
Justin Birdwell ◽  
Jim J. Wang ◽  
Robert L. Cook
Keyword(s):  
Nuclear Magnetic Resonance ◽  
Organic Matter ◽  
Magnetic Resonance ◽  
Organic Soil ◽  
Nuclear Magnetic

Harvesting and Climate Effects on Organic Matter Characteristics in British Columbia Coastal Forests

2002 ◽  
Vol 31 (2) ◽  
pp. 402-413 ◽  
Author(s):  
C.M. Preston ◽  
J.A. Trofymow ◽  
J. Niu ◽  
C.A. Fyfe
Keyword(s):  
British Columbia ◽  
Organic Matter ◽  
Coastal Forests ◽  
Climate Effects

scholarly journals A global hotspot for dissolved organic carbon in hypermaritime watersheds of coastal British Columbia

2017 ◽  
Vol 14 (15) ◽  
pp. 3743-3762 ◽  
Author(s):  
Allison A. Oliver ◽  
Suzanne E. Tank ◽  
Ian Giesbrecht ◽  
Maartje C. Korver ◽  
William C. Floyd ◽  
...  
Keyword(s):  
British Columbia ◽  
Organic Matter ◽  
Organic Carbon ◽  
Stream Water ◽  
Coastal Ocean ◽  
Stream Discharge ◽  
Coastal Margin ◽  
Doc Concentration ◽  
Small Catchments ◽  
Dom Composition

Abstract. The perhumid region of the coastal temperate rainforest (CTR) of Pacific North America is one of the wettest places on Earth and contains numerous small catchments that discharge freshwater and high concentrations of dissolved organic carbon (DOC) directly to the coastal ocean. However, empirical data on the flux and composition of DOC exported from these watersheds are scarce. We established monitoring stations at the outlets of seven catchments on Calvert and Hecate islands, British Columbia, which represent the rain-dominated hypermaritime region of the perhumid CTR. Over several years, we measured stream discharge, stream water DOC concentration, and stream water dissolved organic-matter (DOM) composition. Discharge and DOC concentrations were used to calculate DOC fluxes and yields, and DOM composition was characterized using absorbance and fluorescence spectroscopy with parallel factor analysis (PARAFAC). The areal estimate of annual DOC yield in water year 2015 was 33.3 Mg C km−2 yr−1, with individual watersheds ranging from an average of 24.1 to 37.7 Mg C km−2 yr−1. This represents some of the highest DOC yields to be measured at the coastal margin. We observed seasonality in the quantity and composition of exports, with the majority of DOC export occurring during the extended wet period (September–April). Stream flow from catchments reacted quickly to rain inputs, resulting in rapid export of relatively fresh, highly terrestrial-like DOM. DOC concentration and measures of DOM composition were related to stream discharge and stream temperature and correlated with watershed attributes, including the extent of lakes and wetlands, and the thickness of organic and mineral soil horizons. Our discovery of high DOC yields from these small catchments in the CTR is especially compelling as they deliver relatively fresh, highly terrestrial organic matter directly to the coastal ocean. Hypermaritime landscapes are common on the British Columbia coast, suggesting that this coastal margin may play an important role in the regional processing of carbon and in linking terrestrial carbon to marine ecosystems.

scholarly journals Fertilidade do solo como indicador do efeito de borda em fragmento florestal, Vitória da Conquista, Bahia

2016 ◽  
Vol 11 (4) ◽  
pp. 185
Author(s):  
Danilo Brito Novais ◽  
Joilson Silva Ferreira ◽  
Patrícia Anjos Bittencourt Barreto
Keyword(s):  
Organic Matter ◽  
Organic Carbon ◽  
Soil Fertility ◽  
Edge Effect ◽  
Base Saturation ◽  
Forest Fragment ◽  
Chemical Attributes ◽  
The One ◽  
Composite Samples

Com a expansão da agricultura as florestas têm sido fragmentadas, modificando a dinâmica dos seus processos refletindo na fertilidade do solo. Esse estudo teve como objetivo avaliar o efeito de borda na fertilidade do solo em um fragmento florestal na região Sudoeste da Bahia. Para isso a área foi dividida em faixas verticais iniciando 50 metros após a borda, adentrando até 300 metros no fragmento. Em cada uma das faixas foram tomadas 3 amostras compostas nas profundidades de 0-5, 5-10, 10-20 cm. Analisando os atributos químico e calculando a soma de bases, CTC a pH7 e a saturação por bases (V%). Também foram quantificados os teores de carbono orgânico (COT) nas áreas de estudo. Foram observadas diferenças na fertilidade do solo da borda para o interior do fragmento.  Verificou-se que os atributos Ca2+, H++Al3+, S, T, COT foram os mais sensíveis em relação ao efeito de borda. A área semi-interna (SI) distando 150-200 metros, de maneira geral foi a que apresentou os maiores valores de fertilidade do solo, possivelmente devido aos maiores teores de matéria orgânica acumulada.  Soil fertility as edge effect indicator in a forest fragment, Vitória da Conquista, BahiaAbstract: With the expansion of agriculture forests have been fragmented, changing the dynamics of their processes reflecting soil fertility. This study aimed to evaluate the edge effect on soil fertility in a forest fragment in the Southwest Bahia region. For this area was divided into vertical strips starting 50 meters after the border, entering up to 300 meters in the fragment. In each of the tracks were taken 3 composite samples at depths of 0-5, 5-10, 10-20 cm. Analyzing the chemical attributes and calculating the sum of bases, CTC at pH 7 and base saturation (V%). Also the organic carbon levels were quantified (COT) in the study areas. Differences were observed at the edge of soil fertility into the fragment. It was found that attributes, Ca2+, H++Al3+, S, T, COT were the most sensitive in relation to the edge effect. The semi-internal area (SI) 150-200 meters distant in general was the one with the highest soil fertility values, possibly due to higher levels of accumulated organic matter.

A COMPARISON OF LIME REQUIREMENT METHODS FOR ACID CANADIAN SOILS

1977 ◽  
Vol 57 (3) ◽  
pp. 361-370 ◽  
Author(s):  
M. D. WEBBER ◽  
DIANE CORNEAU ◽  
P. B. HOYT ◽  
M. NYBORG
Keyword(s):  
British Columbia ◽  
Organic Matter ◽  
Soil Ph ◽  
Acid Soils ◽  
Toxic Level ◽  
Laboratory Methods ◽  
Exchangeable Al ◽  
Canadian Soils ◽  
Highly Correlated ◽  
Diagnostic Index

Several laboratory methods for estimating lime requirements of acid soils were compared using 24 soils from Alberta and northeastern British Columbia and 15 from elsewhere in Canada. The Peech, Schofield, Woodruff and SMP (Shoemaker et al. 1971) buffer methods were equally well correlated with lime requirements for raising soil pH to 5.5 or 6, which in turn were highly correlated with the amounts of soluble and exchangeable Al and organic matter in the soils. The SMP buffer method is recommended for use as the diagnostic index of lime requirement to achieve pH 5.5 or 6 because of its speed and simplicity. A refinement is suggested for Alberta and northeastern B.C. soils on the basis that lime need not be added to achieve pH 5.5 but should be added to reduce Al below the toxic level for sensitive crops. The lime requirements to reduce Al in those soils were highly correlated with the amounts of 0.02 M CaCl2-soluble Al they contained and it is recommended that the 0.02 M CaCl2-soluble AI be used as the diagnostic index of lime requirement. Lime requirements related to SMP (pH) and 0.02 M CaCl2-soluble Al are presented.

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