scholarly journals INFLUENCE OF TIME MANAGEMENT IN MODELING OF CURVE RESISTANCE TO THE PENETRATION OF A LATOSOL UNDER DIFFERENT USES AND MANAGEMENT OF PASTURES AND NATIVE WOODLAND

2016 ◽  
Vol 40 (3) ◽  
pp. 519-527 ◽  
Author(s):  
Kathleen Lourenço Fernandes ◽  
Adriana Aparecida Ribon ◽  
João Tavares Filho ◽  
Gustavo Dias Custódio ◽  
Leonardo Rodrigues Barros
Keyword(s):  
Regression Analysis ◽  
Time Management ◽  
Soil Compaction ◽  
Total Porosity ◽  
Soil Resistance ◽  
Independent Variables ◽  
Grazing System ◽  
Native Woodland ◽  
Stepwise Procedure ◽  
Resistance To Penetration

ABSTRACT The soil resistance to penetration study helps in understanding the state of soil compaction, indicating how best to manage it. The present study aimed to verify the influence of time management in modeling curves of resistance to penetration in Oxisol under different uses and management of pastures and woodland in field conditions, using the stepwise procedure. The study was conducted in the Cerrado region. Five (5) systems of uses and management of pastures and native woodland were evaluated: ILPF: crop-livestock-forest integration; ILP: crop-livestock integration; P: Area in the extensive grazing system; MN: native woodland; PIQ: rotated picket. The experiments were assessed for the years 2012/13 and 2013/14. To obtain the models, an analysis with four independent variables was performed: Gravimetric moisture (X1), bulk density (X2), total porosity (X3) and organic matter (X4) and the dependent variable, soil resistance to penetration (Y). The multiple regression analysis by STEPWISE with F of 0.15 was used. The equation that best estimated the resistance to penetration was RP = 14.68 to 0.26 for Native Woodland in layers from 0.20 - 0.40 m with R2 indices of 0.97 in year 1. For year 2, the equation that estimated the resistance to penetration was obtained in the PIQ treatment, PR = - 15.94 - 0.29 PT + 15.87 DS + 0.05 MO. with R2 of 0.94.

scholarly journals COMPACTAÇÃO DO SOLO E INTERVALO HÍDRICO ÓTIMO NO CRESCIMENTO DA PARTE AÉREA E PRODUTIVIDADE DA CULTURA DO MILHO

Irriga ◽  
2008 ◽  
Vol 13 (2) ◽  
pp. 272-287 ◽  
Author(s):  
Ona Da Silva Freddi ◽  
José Frederico Centurion ◽  
Ricardo Garcia Aratani ◽  
Amauri Nelson Beutler
Keyword(s):  
Zea Mays ◽  
Bulk Density ◽  
Soil Compaction ◽  
Dry Matter ◽  
Shoot Growth ◽  
Total Porosity ◽  
Soil Resistance ◽  
Seed Productivity ◽  
Least Limiting Water Range ◽  
Resistance To Penetration

COMPACTAÇÃO DO SOLO E INTERVALO HÍDRICO ÓTIMO NO CRESCIMENTO DA PARTE AÉREA E PRODUTIVIDADE DA CULTURA DO MILHO  Onã da Silva Freddi; José Frederico Centurion; Ricardo Garcia Aratani; Amauri Nelson BeutlerDepartamento de Solos e Adubos, Universidade Estadual Paulista, Faculdade de Ciências Agrárias e Veterináiras, Jaboticabal, SP, [email protected]  1 RESUMO O objetivo do trabalho foi avaliar a compactação do solo proporcionada pelo tráfego de tratores sobre o intervalo hídrico ótimo (IHO) e o crescimento e produtividade do milho em um Latossolo Vermelhode textura argilosa. Os tratamentos foram constituídos por cinco intensidades de compactação e quatro repetições em delineamento inteiramente casualizado. Foram coletadas amostras indeformadas de solo nas camadas de 0,02–0,05, 0,08–0,11, 0,15–0,18 e 0,22-0,25 mpara determinação da macroporosidade, microporosidade, porosidade total, densidade do solo, resistência à penetração e o IHO. Os parâmetros da cultura avaliados foram à altura das plantas e inserção da primeira espiga, o diâmetro do colmo, o número de espigas por planta, a massa seca das plantas e de 1000 grãos e a produtividade. A compactação do solo restringiu todos os parâmetros da cultura avaliados com exceção apenas para o número de espigas e a massa de 1000 grãos. O IHO foi reduzido pela resistência do solo à penetração mesmo no tratamento com solo preparado com densidade média de 1,12 Mg m-3. Apenas o tratamento com quatro passadas do trator de 11 Mg apresentou densidade do solo acima da densidade crítica determinada no IHO, que foi de 1,37 Mg m-3, no qual a produtividade de milho foi significativamente menor. UNITERMOS: Zea mays, resistência do solo à penetração, densidade do solo  FREDDI, O. S.; CENTURION, J. F.; ARATANI, R. G; BEUTLER, A. N. SOIL COMPACTION AND LEAST LIMITING WATER RANGE ON CORN SHOOT GROWTH AND SEED PRODUCTIVITY  2 ABSTRACT The aim of this work was to evaluate the effect of soil compaction caused by tractor wheel traffic on the limiting water range (LLWR), shoot growth and levels of compaction and four replications in a completely randomized experimental design. Soil samples with preserved structure were collected in the layers: 0.02-0.05; 0.08-0.11; 0.15-0.18 and 0.22-0.25m to determine macroporosity, microporosity, total porosity, bulk density, resistance to penetration and LLWR. The evaluated corn parameters were: plant and first spike height, steam diameter, number of spikes per plant, plant dry matter, dry matter of 1000 seeds and seed productivity. The soil compaction restricted all corn parameters except the number of spikes per plant and dry matter of 1000 seeds. The LLWR was reduced by the soil resistance to penetration, even in the tilled soil with bulk density of 1.12 Mg m-3. Only the treatment with 11 Mg tractor, repeated four times on the area, demonstrated bulk density above critical bulk density in the LLWR that was 1.37 Mg m-3, where the seed productivity was significantly smaller. KEY WORDS: Zea mays, soil resistance to penetration, bulk density

scholarly journals Soil resistance to penetration and least limiting water range for soybean yield in a haplustox from Brazil

2005 ◽  
Vol 48 (6) ◽  
pp. 863-871 ◽  
Author(s):  
Amauri Nelson Beutler ◽  
José Frederico Centurion ◽  
Alvaro Pires da Silva
Keyword(s):  
Water Content ◽  
Soil Compaction ◽  
Dry Matter ◽  
Field Capacity ◽  
Soil Resistance ◽  
Soybean Yield ◽  
Randomized Experimental Design ◽  
Least Limiting Water Range ◽  
Dry Matter Weight ◽  
Resistance To Penetration

The objective of this study was determine the resistance to penetration (PR), least limiting water range (LLWR) and critical bulk density (Db-crit) for soybean yield in a medium-textured oxisol (Haplustox). The treatments represented the soil compaction by passing a tractor over the site 0, 1, 2, 4, and 6 times, with 4 replications in a randomized experimental design. Samples were collected from 0.02-0.05, 0.07-0.10 and 0.15-0.18 m depths. Soybean (Glycine max cv. Embrapa 48) was sowed in December 2002. Plant height, number of pods, aerial dry matter, weight of 100 seeds, and the yield in 3.6 m² plots were recorded. Soybean yield started reduction at the PR of 0.85 MPa and Db of 1.48 Mg m-3. The LLWR was limited in highest part by water content at field capacity (0.01 MPa tension) and in lowest part by water content at PRcrit, achieved the Db-crit to yield at 1.48 Mg m-3.

Soil Management in the Physical Attributes and the Wheat Crop Irrigated Productivity

2019 ◽  
pp. 1-11
Author(s):  
Pedro Silvério Xavier Pereira ◽  
Aloisio Bianchini ◽  
Dryelle Sifuentes Pallaoro ◽  
Wininton Mendes da Silva ◽  
Rodrigo Fernandes Daros ◽  
...  
Keyword(s):  
Block Design ◽  
Soil Management ◽  
Total Porosity ◽  
Management Systems ◽  
Wheat Crop ◽  
Soil Resistance ◽  
Soil Density ◽  
Physical Attributes ◽  
Irrigated Wheat ◽  
Resistance To Penetration

The objective of this work was the influence of three management systems on the physical attributes and productivity of irrigated wheat, cultivar BRS-254, in the city of Tangará da Serra, MT, Brazil. The experimental design was a randomized block design in split plots, with eight replications, being considered as plots the three systems of soil management: Conventional management (MC) with two gradations (one heavy and one light); minimum management (MM) with light harrowing; and direct seeding (SD). As a subplot: two layers of soil (0 to 10 cm and 10 to 20 cm) and two seasons, being at 42 and 97 days after sowing (DAS) of wheat. The soil physical attributes evaluated were: macro and microporosity, total porosity, soil density and soil resistance to penetration. The yield of wheat crop was also evaluated. For the effects of MC, MM and SD, of the soil layers and DAS in the parameters macroporosity, microporosity and total soil porosity the MC and MM provided higher values ​​of macroporosity and microporosity decrease at 42 DAS. The macroporosity was higher in the layer up to 10 cm and the microporosity in the 20 cm layer at both the 42 and the 97 DAS. The aeration capacity of the soil followed in ascending order in the management systems SD <MC <MM. In SD there was a significant increase in macroporosity from 42 to 97 DAS. Microporosity presented higher value at 97 DAS. Total porosity, as well as macroporosity, presented the highest value at 42 DAS. For the effects on soil density at 42 DAS it was observed that the lowest density value was found in the MM followed by MC. At 97 DAS, the density values ​​practically returned to the initial value before the management intervention. It was verified that the soil density at the end of the crop cycle had an average value around 1.02 kg dm3. At 42 and 97 DAS the lowest soil density value was found in the 0 to 10 cm layer. In the 10 to 20 cm layer at 42 DAS, the SD had the highest soil density value in relation to the treatments studied, but at 97 DAS the SD had the lowest density value. For the effects on soil penetration resistance it was observed that soil resistance to penetration between MM and MC always remained below 2 MPa. The resistance curve showed that the soil rotation was efficient up to 10 cm depth, as they presented values ​​lower than those found for SD, which presented resistance values ​​between 1.5 and 2 MPa. For the effects on yield of irrigated wheat, the use of MM and SD as a way to reduce soil compaction did not contribute to the increase of yield of irrigated wheat. The MC provided higher productivity.

scholarly journals Physical Quality of an Oxisol in Different Agricultural Systems in Brazilian Cerrado

2018 ◽  
Vol 10 (7) ◽  
pp. 46
Author(s):  
Diego Dos Santos Pereira ◽  
Rafael Montanari ◽  
Christtiane Fernandes Oliveira ◽  
Jean Carlos de Almeida Ramos ◽  
Alan Rodrigo Panosso ◽  
...  
Keyword(s):  
Bulk Density ◽  
Total Porosity ◽  
Forest Plantations ◽  
Soil Resistance ◽  
Brazilian Cerrado ◽  
Physical Quality ◽  
Soil Physical Quality ◽  
The Impact ◽  
Resistance To Penetration

The soil physical quality is a way of evaluating the current condition of forest plantations that is growing in the southeast region of Mato Grosso do Sul State. In this sense, this work aimed to evaluate the impact of the forest plantations on the physical quality of an Oxisol (Haplic Acrustox) in Cerrado. The experiment was conducted in the Experimental area of the Teaching and Research Farm, of the Engineering college of Ilha Solteira (UNESP), located in the city of Selvíria-MS, situated in the conditions of the Brazilian Cerrado. The soil samples were collected at depths of 0.00-0.10; 0.10-0.20; 0.20-0.30 and 0.30-0.40 m in three areas cultivated for 30 years: area (1) Pine forest (Pinus caribaea var. hondurensis); (2) Eucalyptus forest (Eucalyptus camaldulensis); (3) Reforested ciliary forest, being used a completely randomized design, with 25 replications and 3 treatments. The analyzed attributes of the soil was: macroporosity (Ma), microporosity (Mi), total porosity (TP), bulk density (BD), real particle (RP), soil resistance to penetration (PR), gravimetric moisture (GM), volumetric moisture (VM) and sand, silt and clay contents. The three evaluated areas presented macroporosity below the critical limit (0.100 m³ m-³), thereby impairing the root development. The three evaluated areas affected the physical quality of the soil. Being the physical attributes that most influenced in the reduction of the soil physical quality was the bulk density, total porosity, microporosity, macroporosity and soil resistance to penetration.

Soil compaction associated with cut-to-length and whole-tree harvesting of a coniferous forest

2009 ◽  
Vol 39 (5) ◽  
pp. 976-989 ◽  
Author(s):  
Sang-Kyun Han ◽  
Han-Sup Han ◽  
Deborah S. Page-Dumroese ◽  
Leonard R. Johnson
Keyword(s):  
Soil Moisture ◽  
Soil Compaction ◽  
Prediction Models ◽  
Coniferous Forest ◽  
Soil Resistance ◽  
High Soil Moisture ◽  
Harvesting Systems ◽  
Whole Tree Harvesting ◽  
Resistance To Penetration ◽  
Whole Tree

The degree and extent of soil compaction, which may reduce productivity of forest soils, is believed to vary by the type of harvesting system, and a field-based study was conducted to compare soil compaction from cut-to-length (CTL) and whole-tree (WT) harvesting operations. The CTL harvesting system used less area to transport logs to the landings than did the WT harvesting system (19%–20% vs. 24%–25%). At high soil moisture levels (25%–30%), both CTL and WT harvestings caused a significant increase of soil resistance to penetration (SRP) and bulk density (BD) in the track compared with the undisturbed area (p < 0.05). In the center of trails, however, only WT harvesting resulted in a significant increase of SRP and BD compared with the undisturbed area (p < 0.05). Slash covered 69% of the forwarding trail area in the CTL harvesting units; 37% was covered by heavy slash (40 kg·m–2) while 32% was covered by light slash (7.3 kg·m–2). Heavy slash was more effective in reducing soil compaction in the CTL units (p < 0.05). Prediction models were developed that can be used to estimate percent increases in SRP and BD over undisturbed areas for both CTL and WT harvesting systems.

scholarly journals Compaction and Physical Attributes of the Soil After the Development of Cover Plants

2018 ◽  
Vol 10 (7) ◽  
pp. 206 ◽  
Author(s):  
Romário Pimenta Gomes ◽  
Anderson Cristian Bergamin ◽  
Laércio Santos Silva ◽  
Milton César Costa Campos ◽  
Vínicius Augusto Filla ◽  
...  
Keyword(s):  
Bulk Density ◽  
Cover Crops ◽  
Soil Depth ◽  
Soil Management ◽  
Total Porosity ◽  
Grass Species ◽  
Soil Protection ◽  
Soil Resistance ◽  
Physical Attributes ◽  
Resistance To Penetration

Compaction problems in heavily tilled soils have been commonly mitigated with the use of cover plants. Aiming to evaluate the effects of compaction on the physical properties of a plyntic Haplic-Alitic Cambisol soil after development of different cover crops, a complete randomized blocks design experiment, with 3 × 3 factorial arrangement and four replications, was conducted. Treatments consisted of cultivation of two legume species, crotalaria (Crotalaria juncea L.) and stylosanthes cv. Campo Grande (Estilosantes capitata + Estilosantes macrocephala) and a grass species, brachiaria (Urochloa brizhantha cv. Marandu), subjected to soil compaction: CM–Conventional soil management (tillage) without additional compaction; CMc4 and CMc8–conventional soil management with additional compaction using a 6 Mg tractor in four and eight wheel passes. Conventional management with additional compaction does not affect significantly the physical attributes at a soil depth of 0.10-0.20 m, and only the soil moisture does not differ according to the soil management, irrespective of the depth and kind of cover plant. Traffic levels in four passes result in an increased soil bulk density and macroporosity in the 0.0-0.05 m, and in soil resistance to penetration and total porosity in the layer up to 0.10 m. Cover crops are important in maintaining soil physical quality to reduce the negative effects of compacting forces, especially to stylosanthes cv. Campo Grande that provided greater soil protection in systems with or without addition of compaction, conditioning the lowest values of bulk density and soil resistance to penetration.

scholarly journals INTERVALO HÍDRICO ÓTIMO E A PRODUÇÃO DE SOJA E ARROZ EM DOIS LATOSSOLOS

Irriga ◽  
2004 ◽  
Vol 9 (2) ◽  
pp. 181-192 ◽  
Author(s):  
Amauri Nelson Beutler ◽  
José Frederico Centurion ◽  
Alvaro Pires da Silva
Keyword(s):  
Oryza Sativa ◽  
Glycine Max ◽  
Bulk Density ◽  
Soil Compaction ◽  
Functional Relation ◽  
Water Retention Curve ◽  
Root Penetration ◽  
Rice Soil ◽  
Soil Resistance ◽  
Resistance To Penetration

INTERVALO HÍDRICO ÓTIMO E A PRODUÇÃO DE SOJA E ARROZ EM DOIS LATOSSOLOS   Amauri Nelson Beutler1; José Frederico Centurion1-2; Álvaro Pires da Silva2     1Faculdade de Ciências Agrárias e Veterinárias, Universidade Estadual Paulista, Jaboticabal, SP, [email protected] Superior de Agricultura Luiz de Queiroz , Universidade de São Paulo, Piracicaba, SP.   1 RESUMO   Os objetivos deste estudo foram determinar o IHO em Latossolo Vermelho textura média (LVd) e argiloso (LVef) para estabelecer sua relação funcional com a produção de grãos de soja e arroz. Foram coletadas amostras de solo na camada de 0-0,20 m e passadas em peneira de 0,004 m de abertura de malha. Para a determinação do IHO, estabeleceram-se, em vasos (0,20 m de altura e 0,25 m de diâmetro), três níveis de compactação do solo. Foram coletadas 45 amostras indeformadas para determinação da curva de resistência do solo à penetração, da curva de retenção de água, da densidade do solo e do IHO. Para o estudo de crescimento das plantas, estabeleceu-se um experimento com quatro níveis de compactação do solo em vasos, nos quais foram determinados os valores de resistência do solo à penetração e de densidade do solo limitantes à produção de soja e arroz. Em relação ao IHO, os resultados indicaram que a amplitude foi maior no LVef comparado ao LVd. A densidade do solo crítica foi alterada com o valor de resistência à penetração limitante inserido no modelo do IHO, sendo, em geral, superior a densidade limitante a produção de soja e arroz, no LVd, e inferior no LVef.  UNITERMOS: conteúdo de água, compactação do solo, Glycine max, Oryza sativa.   BEUTLER, A.N.; CENTURION, J.F.; SILVA, A.P.LEAST LIMITING WATER RANGE AND YIELD OF SOYBEAN AND RICE IN TWO OXISSOLS  2 ABSTRACT  The objectives of this study were determine the Least limiting water range (LLWR) of a Haplustox medium texture soil(LVd) and Eutruxtox clayey soil(LVef) and to establish its functional relation with the yield of soybean and rice. Soil samples were collected at the depth of  0-0.20 m and then sieved in 0.004 m mesh sieve. Three levels of soil compaction in pots (0.20 m high and 0.25 m diameter) were established to determine LLWR. 45 undisturbed samples were collected to determine soil resistance to root penetration and soil water retention curve, bulk density and the LLWR. For the study of plant growth, an experiment with four levels of soil compaction was established in 0.20 m high x 0.25 m diameter pots; then  the values for resistance to penetration and critical bulk density to yield of soybean and rice were determined. In relation  to the LLWR, the results indicated that the amplitude was higher in LVef compared  to the LVd. The critical bulk density was modified with the limit value for soil resistance to penetration inserted in the model of the LLWR, and was, in general, superior to the limit bulk density to yield of soybean and rice in Haplustox whereas it was  inferior in Eutruxtox.  KEYWORDS: Water content, soil compaction, Glycine max, Oryza sativa

scholarly journals Resistance of soil to penetration as a parameter indicator of subsolation in crop areas of sugar cane

2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Aline Barbosa Arruda ◽  
Rodrigo Fernandes de Souza ◽  
Gustavo Henrique Mendes Brito ◽  
Jadson Belém de Moura ◽  
Manoel Henrique Reis de Oliveira ◽  
...  
Keyword(s):  
Soil Compaction ◽  
Diagnostic Method ◽  
Penetration Resistance ◽  
Soil Resistance ◽  
Agricultural Machinery ◽  
Compacted Soil ◽  
Soil Preparation ◽  
Critical Resistance ◽  
Resistance Value ◽  
Resistance To Penetration

AbstractSugarcane is a very important economic crop that relies heavily on agricultural machinery, which contributes to soil compaction and a consequent decline in productivity. Subsoiling operation reduces the problems caused by compression; however, it is necessary to know its location and intensity. Accordingly, the aim of this work is to present a compression diagnostic method based on soil resistance to penetration as the parameter that indicates need for intervention in the subsoil. Measurements of penetration resistance was carried out in areas of sugarcane, located in the municipalities of Goianésia, Barro Alto and Santa Isabel, in the Brazilian state of Goiás. The Falker penetrometer (PLG 1020) was used, adjusted to a maximum depth of 40 cm and adopted as a critical resistance value of 4.0 MPa. The data were interpolated using kriging and adjusted in AutoCAD 2013 (Autodesk). The methodology proved effective in areas of compacted soil, and the surface layer had less resistance. The reduction in soil preparation was 96.54% and when considering the topographic adjustments, the reduction was 74.07%, showing the viability and importance of the diagnosis to show the proper management.

Geometric Data of Hallux Valgus Feet

1996 ◽  
Vol 17 (9) ◽  
pp. 548-554 ◽  
Author(s):  
Kenneth S. Lamur ◽  
Anton Huson ◽  
Chris J. Snijders ◽  
Rob Stoeckart
Keyword(s):  
Hallux Valgus ◽  
Least Squares Method ◽  
Metatarsal Bone ◽  
Flexor Hallucis Longus ◽  
Independent Variables ◽  
First Metatarsal ◽  
Linear Dependency ◽  
Geometric Data ◽  
Longus Muscle ◽  
Stepwise Procedure

The aim of this study is to find basic quantitative geometric data that may contribute to the understanding of the etiology of hallux valgus. Embalmed specimens with existing hallux valgus (N = 39) were dissected; 28 variables were measured with a Vernier caliper gauge and toe goniometer. Correlations between pairs of independent variables were calculated. Linear dependency of the hallux angle, varus angle, and the width of the forefoot on a number of independent variables was analyzed by multiple linear regression. A least squares method and a stepwise procedure were used. The distance from the tendon of the flexor hallucis longus muscle to the head of the first metatarsal bone explains more than other variables the variation in hallux angle and width of the forefoot. A widened forefoot is significantly correlated with both hallux and varus angles. The interrelation of the predictor parameters illustrates the complicated hallux valgus phenomenon.

Correlation between FA and ADC, number and length of the periprostatic neurovascular fibers

2021 ◽  
pp. 039156032110637
Author(s):  
Valerio Di Paola ◽  
Angelo Totaro ◽  
Giacomo Avesani ◽  
Benedetta Gui ◽  
Andrea Boni ◽  
...  
Keyword(s):  
Regression Analysis ◽  
Linear Regression ◽  
Negative Correlation ◽  
Multivariate Regression ◽  
Linear Regression Analysis ◽  
Multivariate Linear Regression ◽  
Multivariate Linear Regression Analysis ◽  
Independent Variables ◽  
Fiber Tracts ◽  
Good Agreement

Purpose: Our aim was to explore the relation between FA and ADC, number and length of the periprostatic neurovascular fibers (PNF) by means of 1.5 T Diffusion Tensor Imaging (DTI) imaging through a multivariate linear regression analysis model. Methods: For this retrospective study, 56 patients (mean age 63.5 years), who underwent 1.5-T prostate MRI, including DTI, were enrolled between October 2014 and December 2018. Multivariate regression analysis was performed to evaluate the statistically significant correlation between FA values (dependent variable) and ADC, the number and the length of PNF (independent variables), if p-value <0.05. A value of 0.5 indicated poor agreement; 0.5–0.75, moderate agreement; 0.75–0.9, good agreement; 0.61–0.80, good agreement; and 0.9–1.00, excellent agreement. Results: The overall fit of the multivariate regression model was excellent, with R2 value of 0.9445 ( R2 adjusted 0.9412; p < 0.0001). Multivariate linear regression analysis showed a statistically significant correlation ( p < 0.05) for all the three independent variables. The r partial value was −0.9612 for ADC values ( p < 0.0001), suggesting a strong negative correlation, 0.4317 for the number of fiber tracts ( p < 0.001), suggesting a moderate positive correlation, and −0.306 for the length of the fiber tracts ( p < 0.05), suggesting a weak negative correlation. Conclusions: Our multivariate linear regression model has demonstrated a statistically significant correlation between FA values of PNF with other DTI parameters, in particular with ADC.

Sign in / Sign up

Export Citation Format

Share Document