scholarly journals Plasticidade fenotípica de Psidium cattleianum (Myrtaceae) em ambiente insular e continental na baía Babitonga em São Francisco do Sul, Santa Catarina

2021 ◽  
Vol 14 (2) ◽  
pp. 1025
Author(s):  
Andressa Cristina França ◽  
João Carlos Ferreira Melo Júnior ◽  
Patrícia Soffiatti
Keyword(s):  
Phenotypic Plasticity ◽  
Environmental Changes ◽  
Statistical Treatment ◽  
Organic Matter Content ◽  
Matter Content ◽  
Environmental Filters ◽  
Santa Catarina ◽  
Chlorophyll Contents ◽  
Psidium Cattleianum ◽  
Plastic Potential

A plasticidade fenotípica permite aos vegetais a sobrevivência e sucesso reprodutivo em meios com distintas condições ambientais. Ambientes insulares são altamente restritivos devido à características como alta salinidade e incidência luminosa e deficiência nutricional do solo, as quais atuam como filtro ambiental para o estabelecimento de espécies. O presente estudo objetivou avaliar a plasticidade fenotípica de Psidium cattleianum (Myrtaceae), comparando populações co-ocorrentes em ilha e continente na Baía Babitonga/SC. Para tanto, foram selecionados 10 indivíduos em cada ambiente, dos quais foram coletadas 35 folhas maduras e de sol para análises morfoanatômicas e fisiológicas, posterior tratamento estatístico em ambiente R e cálculo do Índice de Plasticidade fenotípica (IPF). Análise química do solo foi procedida por meio de amostras compostas de 10 coletas por ambiente. O ambiente insular apresenta solo menos ácido, com maior conteúdo de matéria orgânica, salinidade e disponibilidade de água quando comparado ao continente, porém com menor capacidade de troca catiônica (CTC). A intensidade de luz apresentou maior incidência sobre as plantas da ilha. Em razão da heterogeneidade ambiental, diferenças estatisticamente significativas foram registradas para os atributos arquiteturais e morfoanatômicos das populações, representando ajustes funcionais desencadeados por um filtro ambiental. Os três primeiros eixos da PCA explicaram 64,35% da variação de dados, como maior expressão dos atributos de massas fresca e seca, teores de clorofila e espessura do parênquima lacunoso. Para o IPF, todos os atributos avaliados mostraram valores abaixo de 0,3, indicando o baixo potencial plástico entre as populações de P. cattleianum, porém com diferenças nas estratégias ecológicas que otimizam a alocação de recursos nos ambientes estudados. Phenotypic plasticity of co-current Psidium cattleianum (Myrtaceae) in an island and continental environment at Babitonga Bay in São Francisco do Sul, Santa CatarinaA B S T R A C TPhenotypic plasticity allows plants survival and to reproduce successfully in face of environmental changes. This study aimed to investigate, on an individual scale, the response of Psidium cattleianum (Myrtaceae) in two distinct environmental conditions: island and mainland in Babitonga Bay, São Francisco do Sul, Santa Catarina. For this purpose, two populations comprising 10 individuals were selected in each study area, from which 35 mature sun leaves were collected for morphoanatomical and physiological analysis; soil chemical analysis was performed on composed samples formed by 10 collections per area. The statistical treatment was performed in R environment and also the Phenotypic Plasticity Index (IPF) was calculated. The island environment has less acid soils, with higher organic matter content, salinity and water availability when compared to mainland, but with lower cation exchange capacity (CTC), besides higher light intensity. Due to areas heterogeneity, statistically significant differences were recorded for the morphoanatomical and physiological attributes of the populations, representing functional adjustments triggered by environmental filters. The first three axes of the PCA explained 64.35% of the data variation, with greater expression of fresh and dry mass attributes, chlorophyll contents and thickness of spongy parenchyma. For the IPF, all the attributes evaluated showed values below 0.3, indicating the low plastic potential among P. cattleianum populations, but with differences in ecological strategies that optimize resource allocation in the studied environments.Keywords: araçá, environmental heterogeneity, functional adjustments, ombrophilous forest, plastic potential.

scholarly journals Effectiveness of a rapid soil incubation method for determining potential acidity of soils in Rio Grande do Sul, Brazil

2019 ◽  
Vol 49 (2) ◽  
Author(s):  
Gustavo Brunetto ◽  
Rodrigo Otávio Schneider Souza ◽  
Rogério Piccin ◽  
Roque Junior Sartori Bellinaso ◽  
João Kaminski ◽  
...  
Keyword(s):  
Organic Matter Content ◽  
Rio Grande ◽  
Matter Content ◽  
Rio Grande Do Sul ◽  
Santa Catarina ◽  
Ph Values ◽  
Soluble Base ◽  
Santa Maria ◽  
Incubation Method ◽  
Potential Acidity

ABSTRACT: Potential soil acidity can be measured by two methods in the states of Rio Grande do Sul (RS) and Santa Catarina (SC): solution SMP or solution TSM (Buffer Santa Maria). Calibration of these methods is done by incubating soils for long periods (180 days) of CaCO3. The hypothesis of this study is that it is possible to reduce the incubation period in soils by using a soluble base such as calcium hydroxide. The study aimed to estimate potential acidity in a group of soils by moist incubation with Ca(OH)2 (short) as an alternative to the typical method with CaCO3 (long) and relate to the values estimated by the equation used by the Soil Chemistry and Fertility Commission of Rio Grande do Sul and Santa Catarina (CQFS-RS/SC; 2016). Ten soils with sandy texture and low organic matter content were collected at 0-20cm in the Campanha Gaúcha region of the state of RS and incubated for 180 days with doses of CaCO3 equivalent to 0, 25, 50, 75, 100, 125 and 150% of the lime requirement estimated by the solution TSM to raise to pH 6.0. Soils were also incubated for 4 days in an oven at 35ºC with 0.22mol L-1 Ca(OH)2 at doses equivalent to CaCO3. Short incubation of the soil with Ca(OH)2 may substitute long incubation with CaCO3. Also, estimating potential acidity using the equation of the CQFS-RS/SC (2016) overestimated potential acidity in soils with solution TSM pH values lower than 6.0 in this study.

scholarly journals Water retention and availability in soils of the State of Santa Catarina-Brazil: effect of textural classes, soil classes and lithology

2013 ◽  
Vol 37 (6) ◽  
pp. 1535-1548 ◽  
Author(s):  
André da Costa ◽  
Jackson Adriano Albuquerque ◽  
Adriano da Costa ◽  
Patricia Pértile ◽  
Franciani Rodrigues da Silva
Keyword(s):  
Organic Matter ◽  
Cover Crops ◽  
Water Availability ◽  
Water Retention ◽  
Mixed Model ◽  
Organic Matter Content ◽  
Matter Content ◽  
The State ◽  
Santa Catarina ◽  
Alluvial Deposits

The retention and availability of water in the soil vary according to the soil characteristics and determine plant growth. Thus, the aim of this study was to evaluate water retention and availability in the soils of the State of Santa Catarina, Brazil, according to the textural class, soil class and lithology. The surface and subsurface horizons of 44 profiles were sampled in different regions of the State and different cover crops to determine field capacity, permanent wilting point, available water content, particle size, and organic matter content. Water retention and availability between the horizons were compared in a mixed model, considering the textural classes, the soil classes and lithology as fixed factors and profiles as random factors. It may be concluded that water retention is greater in silty or clayey soils and that the organic matter content is higher, especially in Humic Cambisols, Nitisols and Ferralsol developed from igneous or sedimentary rocks. Water availability is greater in loam-textured soils, with high organic matter content, especially in soils of humic character. It is lower in the sandy texture class, especially in Arenosols formed from recent alluvial deposits or in gravelly soils derived from granite. The greater water availability in the surface horizons, with more organic matter than in the subsurface layers, illustrates the importance of organic matter for water retention and availability.

scholarly journals Pedotransfer functions to estimate retention and availability of water in soils of the state of Santa Catarina, Brazil

2013 ◽  
Vol 37 (4) ◽  
pp. 889-910 ◽  
Author(s):  
André da Costa ◽  
Jackson Adriano Albuquerque ◽  
Jaime Antônio de Almeida ◽  
Adriano da Costa ◽  
Rodrigo Vieira Luciano
Keyword(s):  
Organic Matter ◽  
Regression Analysis ◽  
Path Analysis ◽  
Water Retention ◽  
Organic Matter Content ◽  
Soil Surface ◽  
Matter Content ◽  
The State ◽  
Pedotransfer Functions ◽  
Santa Catarina

Studies on water retention and availability are scarce for subtropical or humid temperate climate regions of the southern hemisphere. The aims of this study were to evaluate the relations of the soil physical, chemical, and mineralogical properties with water retention and availability for the generation and validation of continuous point pedotransfer functions (PTFs) for soils of the State of Santa Catarina (SC) in the South of Brazil. Horizons of 44 profiles were sampled in areas under different cover crops and regions of SC, to determine: field capacity (FC, 10 kPa), permanent wilting point (PWP, 1,500 kPa), available water content (AW, by difference), saturated hydraulic conductivity, bulk density, aggregate stability, particle size distribution (seven classes), organic matter content, and particle density. Chemical and mineralogical properties were obtained from the literature. Spearman's rank correlation analysis and path analysis were used in the statistical analyses. The point PTFs for estimation of FC, PWP and AW were generated for the soil surface and subsurface through multiple regression analysis, followed by robust regression analysis, using two sets of predictive variables. Soils with finer texture and/or greater organic matter content retain more moisture, and organic matter is the property that mainly controls the water availability to plants in soil surface horizons. Path analysis was useful in understanding the relationships between soil properties for FC, PWP and AW. The predictive power of the generated PTFs to estimate FC and PWP was good for all horizons, while AW was best estimated by more complex models with better prediction for the surface horizons of soils in Santa Catarina.

scholarly journals Interplay between eutrophication and climate warming on bacterial communities in coastal sediments differs depending on water depth and oxygen history

2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Laura Seidel ◽  
Elias Broman ◽  
Stephanie Turner ◽  
Magnus Ståhle ◽  
Mark Dopson
Keyword(s):  
Relative Abundance ◽  
Water Depth ◽  
Bacterial Communities ◽  
Environmental Changes ◽  
Organic Matter Content ◽  
Matter Content ◽  
Coastal Sediments ◽  
Rrna Gene ◽  
Low Oxygen ◽  
Bacterial Populations

AbstractCoastal aquatic systems suffer from nutrient enrichment, which results in accelerated eutrophication effects due to increased microbial metabolic rates. Climate change related prolonged warming will likely accelerate existing eutrophication effects, including low oxygen concentrations. However, how the interplay between these environmental changes will alter coastal ecosystems is poorly understood. In this study, we compared 16S rRNA gene amplicon based bacterial communities in coastal sediments of a Baltic Sea basin in November 2013 and 2017 at three sites along a water depth gradient with varying bottom water oxygen histories. The shallow site showed changes of only 1.1% in relative abundance of bacterial populations in 2017 compared to 2013, while the deep oxygen-deficient site showed up to 11% changes in relative abundance including an increase of sulfate-reducing bacteria along with a 36% increase in organic matter content. The data suggested that bacterial communities in shallow sediments were more resilient to seasonal oxygen decline, while bacterial communities in sediments subjected to long-term hypoxia seemed to be sensitive to oxygen changes and were likely to be under hypoxic/anoxic conditions in the future. Our data demonstrate that future climate changes will likely fuel eutrophication related spread of low oxygen zones.

HEAVY METAL SPECIATION IN BOTTOM SEDIMENTS OF THE VYSHNEVOLOTSKY RESERVOIR

2018 ◽  
pp. 46-54
Author(s):  
O. A. Lipatnikova
Keyword(s):  
Heavy Metal ◽  
Organic Matter ◽  
Bottom Sediments ◽  
Metal Speciation ◽  
Organic Matter Content ◽  
Water Reservoir ◽  
Matter Content ◽  
Heavy Metal Speciation ◽  
Mobile Forms ◽  
Manganese Hydroxides

The study of heavy metal speciation in bottom sediments of the Vyshnevolotsky water reservoir is presented in this paper. Sequential selective procedure was used to determine the heavy metal speciation in bottom sediments and thermodynamic calculation — to determine ones in interstitial water. It has been shown that Mn are mainly presented in exchangeable and carbonate forms; for Fe, Zn, Pb и Co the forms are related to iron and manganese hydroxides is played an important role; and Cu and Ni are mainly associated with organic matter. In interstitial waters the main forms of heavy metal speciation are free ions for Zn, Ni, Co and Cd, carbonate complexes for Pb, fulvate complexes for Cu. Effects of particle size and organic matter content in sediments on distribution of mobile and potentially mobile forms of toxic elements have been revealed.

Physico-Chemical Properties of Soil Collected from Chandrabhaga River in Kalmeshwar, Nagpur, Maharashtra

2020 ◽  
Vol 07 (02) ◽  
pp. 1-3
Author(s):  
Amita M Watkar ◽  
Keyword(s):  
Organic Matter ◽  
Soil Quality ◽  
Agricultural Land ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Matter Content ◽  
Soil Attributes ◽  
Essential Components ◽  
Agricultural Land Management ◽  
Physical And Chemical

Soil, itself means Soul of Infinite Life. Soil is the naturally occurring unconsolidated or loose covering on the earth’s surface. Physical properties depend upon the amount, size, shape, arrangement, and mineral composition of soil particles. It also depends on the organic matter content and pore spaces. Chemical properties depend on the Inorganic and organic matter present in the soil. Soils are the essential components of the environment and foundation resources for nearly all types of land use, besides being the most important component of sustainable agriculture. Therefore, assessment of soil quality and its direction of change with time is an ideal and primary indicator of sustainable agricultural land management. Soil quality indicators refer to measurable soil attributes that influence the capacity of a soil to function, within the limits imposed by the ecosystem, to preserve biological productivity and environmental quality and promote plant, animal and human health. The present study is to assess these soil attributes such as physical and chemical properties season-wise.

UPAYA MEMPERTAHANKAN BUNGA DAN FRUIT SET TANAMAN CABAI (Capsicum annum L.) PADA LAHAN ULTISOL MELALUI PEMBERIAN LUMPUR LAUT DAN PUPUK KANDANG

2017 ◽  
Vol 13 (2) ◽  
pp. 74-77
Author(s):  
Imelda J Lawalatta ◽  
Francina Matulessy ◽  
Meitty L Hehanussa
Keyword(s):  
Fruit Set ◽  
Agricultural Land ◽  
Mineral Soil ◽  
Organic Matter Content ◽  
Nutrient Deficiency ◽  
Matter Content ◽  
Infrastructure Development ◽  
Capsicum Annum ◽  
Factor Effect ◽  
Marine Mud

Chili (Capsicum annum L.) often experience the highest price fluctuations in Indonesia. This is caused by the production that is often disrupted in certain months, especially in the months in the rainy season due to flowers and fruits that fall before the harvest. Since agricultural land has changed its function for infrastructure development, marginal land (Ultisol) is used. The ultisol problem is: high acidity, low organic matter content, nutrient deficiency important for plants (eg N, P, Ca, Mg and Mo) and high solubility of Al, Fe and Mn. The provision of organic materials such as manure and marine mud will overcome the problem of acid-rich mineral soil and play an important role in improving, increased and maintaining sustainable land productivity. Research results for chili flower significantly. the highest number of flowers found in the treatment of L0P3, L1P2, L1P3 and L2P3 that is > 60 flower/plant. There was a single factor effect for the amount of fruit, mostly found in L3 treatment (600 ton/ha marine mud) that is 22.36 fruit/plant. The treatment of manure significantly influenced the formation of the most fruit set in the treatment of P0 and P2 (without manure and manure 20 ton/ha) that is 77.60% and 70.,45%. Keywords: Ultisol, Marine mud, Manure, Flowers and Fruit sets   ABSTRAK Tanaman cabai besar (Capsicum annum L.) sering mengalami fluktuasi harga paling tinggi di Indonesia. Hal tersebut disebabkan oleh produksi yang sering terganggu pada bulan tertentu terutama pada bulan-bulan di musim penghujan dikarenakan bunga dan buah yang rontok sebelum panen. Karena lahan pertanian banyak beralih fungsinya untuk pembangunan infrastuktur, maka digunakan lahan marginal (Ultisol). Masalah ultisol ialah: kemasaman tinggi, kadar bahan organik yang rendah, kekurangan unsur hara penting bagi tanaman (contoh: N, P, Ca, Mg dan Mo) serta tingginya kelarutan Al, Fe dan Mn. Pemberian bahan organik seperti pupuk kandang dan Lumpur laut akan mengatasi persoalan tanah mineral masam berkadar Al tinggi dan berperan penting dalam memperbaiki, meningkatkan serta mempertahankan produktifitas lahan secara berkelanjutan Hasil Penelitian untuk jumlah bunga cabai berpengaruh signifikan. jumlah bunga terbanyak terdapat pada perlakuan L0P3, L1P2, L1P3 dan L2P3 yaitu > 60 bunga/tanaman. Terjadi pengaruh faktor tunggal untuk jumlah buah, terbanyak terdapat pada perlakuan L3 ( 600 ton/ha lumpur laut) yaitu 22,36 buah/tanaman. Perlakuan pupuk kandang berpengaruh signifikan Pembentukan fruit set terbanyak pada perlakuan P0 dan P2 (tanpa pupuk kandang dan pupuk kandang 20 ton/ha) yaitu 77,60% dan 70,45%. Kata kunci: Ultisol, Lumpur Laut, Pupuk Kandang, Bunga dan Fruit set

scholarly journals Soil nitrogen supply of peat grasslands estimated by degree days and soil organic matter content

2020 ◽  
Vol 117 (3) ◽  
pp. 351-365
Author(s):  
J. Pijlman ◽  
G. Holshof ◽  
W. van den Berg ◽  
G. H. Ros ◽  
J. W. Erisman ◽  
...  
Keyword(s):  
Organic Matter ◽  
Soil Organic Matter ◽  
Soil Nitrogen ◽  
Organic Matter Content ◽  
Matter Content ◽  
Nitrogen Supply ◽  
Degree Days ◽  
Soil Organic Matter Content ◽  
Soil Nitrogen Supply

scholarly journals Microbial Respiration and Enzyme Activity Downstream from a Phosphorus Source in the Everglades, Florida, USA

Land ◽  
2021 ◽  
Vol 10 (7) ◽  
pp. 696
Author(s):  
Sanku Dattamudi ◽  
Saoli Chanda ◽  
Leonard J. Scinto
Keyword(s):  
Nutrient Dynamics ◽  
Microbial Respiration ◽  
Organic Matter Content ◽  
Physicochemical Analysis ◽  
Matter Content ◽  
Enzyme Assays ◽  
Co2 Efflux ◽  
Soil Organic Matter Content ◽  
Phosphorus Source ◽  
P Distribution

Northeast Shark River Slough (NESS), lying at the northeastern perimeter of Everglades National Park (ENP), Florida, USA, has been subjected to years of hydrologic modifications. Construction of the Tamiami Trail (US 41) in 1928 connected the east and west coasts of SE Florida and essentially created a hydrological barrier to southern sheet flow into ENP. Recently, a series of bridges were constructed to elevate a portion of Tamiami Trail, allow more water to flow under the bridges, and attempt to restore the ecological balance in the NESS and ENP. This project was conducted to determine aspects of soil physiochemistry and microbial dynamics in the NESS. We evaluated microbial respiration and enzyme assays as indicators of nutrient dynamics in NESS soils. Soil cores were collected from sites at certain distances from the inflow (near canal, NC (0–150 m); midway, M (150–600 m); and far from canal, FC (600–1200 m)). Soil slurries were incubated and assayed for CO2 emission and β-glucoside (MUFC) or phosphatase (MUFP) activity in concert with physicochemical analysis. Significantly higher TP contents at NC (2.45 times) and M (1.52 times) sites than FC sites indicated an uneven P distribution downstream from the source canal. The highest soil organic matter content (84%) contents were observed at M sites, which was due to higher vegetation biomass observed at those sites. Consequently, CO2 efflux was greater at M sites (average 2.72 µmoles g dw−1 h−1) than the other two sites. We also found that amendments of glucose increased CO2 efflux from all soils, whereas the addition of phosphorus did not. The results indicate that microbial respiration downstream of inflows in the NESS is not limited by P, but more so by the availability of labile C.

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