Dynamics of leaf transpiration in two contrasting maize (Zea mays L

Slides:



Advertisements
Similar presentations
Z. Liu, B. Dugan, C.A. Masiello, and H. Gonnermann, Rice University
Advertisements

Simulating Cropping Systems in the Guinea Savanna Zone of Northern Ghana with DSSAT-CENTURY J. B. Naab 1, Jawoo Koo 2, J.W. Jones 2, and K. J. Boote 2,
Effects of Salt Stress on the Stem Length of Arabidopsis thaliana Jacob Phillips Undergraduate Student Biology Health Sciences Concentration Department.
“Biochar,” a bit of myth busting
Responses of Sweet Cherry Productivity and Soil Quality to Alternate Groundcover and Irrigation Systems Xinhua Yin 1, Xiaolan Huang 1, and Lynn Long 2.
Effect of Long-term Cattle Manure Application on Soil Test Phosphorus, Organic Carbon and Winter Wheat Grain Yield Natasha Macnack, Peter Omara, Lawrence.
Cover Crops and Biofuels Implications for Soil Characteristics and Plant Development Deanna Boardman October 21, 2009.
TYPES OF SOIL There are three major types of soil, namely; sandy soil, clay soil and loamy soil. SANDY SOIL. Any soil sample that contains sand particles.
Characterization of Soil Resilience as influenced by Organic Management Practices in Perturbed Vertisol Ritesh Saha ICAR- Indian Institute of Soil Science.
INFLUENCES OF IRRIGATION AND N FERTILIZATION ON MAIZE (Zea mays L.) PROPERTIES - Hrvoje PLAVSIC1 - Marko JOSIPOVIC1 - Luka ANDRIC1 - Antun JAMBROVIC1 -
Overview of Soil Properties for Crop Production By J.G. Mexal Department of Plant & Environmental Sciences New Mexico State University.
Mladen Todorovic & Rossella Albrizio (CIHEAM-IAMB, Italy) Ljubomir Zivotic (Institute for Water Management “Jaroslav Cerni”, Belgrade, Serbia) Deficit.
The rice plant-soil-water system Crop and Environmental Sciences Division International Rice Research Institute Los Baños, Philippines.
Impact of Soil Health on Crop Production Francisco J. Arriaga Soil Science Specialist Dept. of Soil Science & UW-Extension.
Making sure we can handle the extremes! Carolyn Olson, Ph.D. 90 th Annual Outlook Forum February 20-21, 2014.
Measuring Soil Physical Properties to Assess Soil Quality Charles W. Raczkowski North Carolina A&T State University Presented at the Soil Quality Workshop.
EFFECTS OF Calliandra calothyrsus and Alnus acuminata GREEN MANURES IN MAIZE PRODUCTION IN THE HIGHLAND VOLCANIC SOILS OF RWANDA Didace HABAMENSHI ISAE.
Comparison of Regional and NuMaSS Fertilizer Rates in On-station and On-farm Trials in Northern Ghana Jesse B. Naab 1, C. Yamoah 2, R. Yost 3 and R.A.
Peter Motavalli Dept. of Soil, Environmental and Atmos. Sci. University of Missouri University of Missouri ADAPTING TO CHANGE:
MODELING THE IMPACT OF IRRIGATION ON NUTRIENT EXPORT FROM AGRICULTURAL FIELDS IN THE SOUTHEASTERN UNITED STATES W. Lee Ellenburg Graduate Research Assistant.
TOTAL AND EXTRACTABLE PHOSPHORUS CONCENTRATIONS AT DIFFERENT DEPTHS IN A SOIL FERTILIZED WITH MANURE R. DA SILVA DÍAS 1, C. A. de ABREU 2, R. M. MESTAS.
Comparing Conventional Tillage and No Till
Results of Long-Term Experiments With Conservation Tillage in Austria Introduction On-site and off-site damages of soil erosion cause serious problems.
Consequences of Aluminum or Ferrous Sulfate Amended Poultry Litter on Concentrations of Aluminum in Plant and Soil Sosten Lungu, Haile Tewolde and Dennis.
AP Environmental Science Soil Resources Living in the Environment, 14th edition, G. Tyler Miller.
Proposed Agriculture Courses Board of Education October 6, 2015.
Modelling Crop Development and Growth in CropSyst
Figure 3. Concentration of NO3 N in soil water at 1.5 m depth. Evaluation of Best Management Practices on N Dynamics for a North China Plain C. Hu 1, J.A.
Effects of parent material and land use on soil phosphorus forms in Southern Belgium Renneson 1 M., Dufey 2 J., Bock 1 L. and Colinet 1 G. 1 University.
Agronomic Spatial Variability and Resolution What is it? How do we describe it? What does it imply for precision management?
Photo: David Brazier/IWMI Photo :Tom van Cakenberghe/IWMI Photo: David Brazier/IWMI Water for a food-secure world W. Mekuria, A. Noble, C.T.
MODELING WATER UPTAKE BY TURFGRASS FOR A USGA ROOT ZONE MODIFIED WITH INORGANIC AMENDMENTS Leonard Githinji, Jacob Dane and Robert Walker, Auburn University,
Managing Tillage and FYM for Enhancing Maize Production and Soil Properties in Mid-hills of Nepal Pudasaini, R. and Pande, K. R. Presenter: Roshan Pudasaini.
NE: No effect. Data were not significantly different from control. (p
AE 152 IRRIGATION & DRAINAGE
Wood ash, the residue remaining from the combustion of bark, sawdust and yard waste for energy generation for forestry product operations, is an effective.
Integrated Nutrient Management (Nutrient Management Plan ) A Series of Lecture By Mr. Allah Dad Khan.
What is AG Biochar Raw & How Can it Help Grow your Business
Water in Soil Learning objectives
Dr. J. P. Deshmukh Shri. S. N. Potkile Shri. P. V. Shingrup
Soil Review Powerpoint
Evaluation of early drought tolerant maize genotypes under low nitrogen conditions Nyasha E. Goredema1, Ms Nakai Goredema2, Ezekia Svotwa1, Gabriel Soropa1,
Update on the Performance of two Southern Highbush Blueberry Cultivars Grafted onto Vaccinium arboreum (Sparkleberry) Rootstocks Bruno Casamali MS Student.
University, Nakhon Pathom, Thailand, 73140
Long term Biochar versus Wood Ash Agronomic Field Trial at 6 months
3RD WASWAC CONFERENCE: Land degradation processes and mechanism
Fungal and Bacterial Dynamics in the Lettuce Rhizosphere Responding to Successive Additions of Cd and Zn. A. M. I. D. Amarakoon * and R. M. C. P. Rajapaksha.
By Muhammad Akhlaq Mudassir Assistant Research Officer
The effect of dry period irrigation on yield of three cassava cultivar
An Agriculture Perspective
Proportion of intermediate diameter roots
Prof. DSc Eng. Zornitsa Popova, Assist. Prof. Dr Eng. Maria Ivanova
Water in Soil Learning objectives
Third International, AGRONOMY CONGRESS Agriculture Diversification, Climate Change Management and Livelihoods November 26-30, 2012, New Delhi, India Hyperspectral.
Topsoil Depth at the Centralia Site
Bioscience conference, Berlin, Germany
The Effect of Biochar on the growth of Quercus serrata and
Arafat Alkhasha Abdulrasoul Al-Omran Anwar Aly
YIELD AND QUALITY OF SWEET CORN (Zea mays L. var
Chemical Properties of a Xerofluvent Soil and Corn Yield (Zea Mays L.)
DROUGHT VULNERABILITY QUANTIFICATION IN BULGARIA THROUGH MODELING CROP PRODUCTIVITY AND IRRIGATION REQUIREMENTS Z. Popova*, М. Ivanova*, L.S.Pereira**,
From: Deficit irrigation for reducing agricultural water use
Soil Formation Soil horizons - layers of soil renewal
The Effects of Biochar on Plant Growth
The rice plant-soil-water system
Using Soil Moisture and Matric Potential Observations to Identify Subsurface Convergent Flow Pathways Qing Zhu, Henry Lin, and Xiaobo Zhou Dept . Crop.
Evangelos Gonias, Derrick Oosterhuis, Androniki Bibi and Bruce Roberts
Crop Growth Model Simulation of G2F Common Hybrids
Setback area relative to drainage area Runoff volume, mean of 4 events
Development of Activated Hydrochar from Paddy Straw
Presentation transcript:

Dynamics of leaf transpiration in two contrasting maize (Zea mays L Dynamics of leaf transpiration in two contrasting maize (Zea mays L.) hybrids under water stress and biochar amendment Leila Romdhane1 , Teofilo Vamerali2, Marianna Bandiera2, Giuseppe Barion2, Giuliano Mosca2 and Leila Radhouane1 1 University of Carthage-Faculty of Sciences of Bizerte / National Institute of Agronomic Research of Tunisia (INRAT) - Tunisia 2 University of Padova, Department of Agronomy, Food, Natural Resources, Animals and the Environment, (DAFNAE) – Legnaro, Padova - Italy Introduction Soil water retention is determined by the distribution and connectivity of pores in the soil matrix, which is largely affected by soil texture, aggregation and soil organic matter content (Brady and Weill, 2004). Biochar, a C-rich material produced by pyrolysis (temperature 300-700 °C, anoxic conditions) of organic biomass, including agricultural wastes, has a higher surface area and greater porosity relative to other types of soil organic materials and therefore can improve soil texture and aggregation, and consequently soil water retention (Kongthod et al., 2015). A pot trial was conducted during summer 2014 at the experiment farm of the University of Padova at Legnaro (NE Italy) in order to follow the dynamics of leaf transpiration in two contrasting maize hybrids with and without biochar addition to the soil in conditions of progressively decreased water availability. Materials and Methods 2 maize hybrids (Pionneer Hi-Bred-Dupont; FAO class 700): Drought tolerant (T): D24 Drought sensitive (S): P1921 2 treatments , 5 replicates ( Fig. 1): Biochar (1% w/w) (BC1%): soil pH 7.88, EC 0.58 mS cm-1 ; 5 kg of soil + 50 g biochar +2.5 g NPK fertilizer (15-15-15) per pot. Untreated controls (C): soil pH=7.55, EC 0.50 mS cm-1 (Fig.1) Growing period: August 11th – October 10th. The effects of water stress were evaluated by calculating the “linear plateau regression” obtained by relating daily relative transpiration (RT) over the fraction of transpirable soil water (FTSW) (Vamerali et al., 2003), as follows: y = a + b * (x - c) * (x <= c) Fig. 1 . Pot trial BC (1% w/w) C Fig. 2. Relationships between relative transpiration (RT) and fraction of transpirable soil water (FTSW) of maize hybrids D24 and P1921 (Plateaux Linear Regression), under progressive water deficit regime under biochar-amended soil (1% w/w) and unamended controls. Coefficients of regression curves are: a = 97,13, b = 0,80, R2 = 85,6% (Untreated D24); a = 97,88, b = 1,69, R2 = 94,33% (Untreated P1921); a = 95,63, b = 1,65, R2 = 92,92% (BC1% D24); a = 93,95, b = 3,87, R2 = 95,49% (BC P1921). Threshold at which RT begins to decline was estimated by the plateau linear regression model as coefficient “c”. Results Results showed that in both hybrids biochar was able to maintain a high rate of transpiration down to low FTSW values. The linear plateau regression model of un-amended controls of D24 start to decline earlier (82 % FTSW value) than in P1921 (45% FTSW value), confirming the water-saving strategy of D24. Instead, soil amended with biochar allowed plants of both hybrids to transpire at their maximum down to lower FTSW, i.e., 45% and 22% in D24 and P1921, respectively (Fig. 2). Conclusions It is concluded that biochar can delay the inhibition of transpiration in condition of limited water availability in agreement with the commonly observed capacity of biochar to improve the water holding capacity, a fact that is attributed to the high surface area of biochar which helps it to increase water retention. Bibliography Vamerali T., Saccomani M., Bona S., Mosca G., Guarise M., Ganis A. (2003). A comparison of root characteristics in relation to nutrient and water stress in two maize hybrids. Plant and soil 255: 157-167. Brady NC, Weil PR. 2004. The nature and properties of soils.??????? KONGTHOD T., THANACHIT S., ANUSONTPORNPERM S., WIRIYAKITNATEEKUL W. (2015). Effects of biochars and other oganic soil amendments on plant nutrient availability in an Ustoxic Quartz ipsamment. Pedosphere 25(5):790 – 798, 2015.