Freshwater is a finite resource that is rapidly becoming more scrutinized in agricultural consumption. Specialty crop producers, especially ornamental crop producers, must continually improve production sustainability, with regards to water resource management, in order to continue to stay economically viable. Soilless substrates were initially developed to have increased porosity and relatively low water holding capacity to ensure container crops would not remain overhydrated after irrigations or rain events. As a result, substrates were selected that are now considered to be in efficient in regards to water resource management. Therefore, to provide growers with additional means to improve production sustainability, soilless substrate hydrology needs be innovated to provide increased water availability while continuing to provide ample air filled porosity to ensure productive and efficient water interactions. Historically, soilless substrates have been characterized using "static" physical properties (i.e. maximum water holding capacity and minimum air-filled porosity). The research herein involves integrating dynamic soilless substrate hydraulic properties to understand how substrate hydrology can be manipulated to design sustainable substrates. This task involved adapting new technologies to analyze hydrological properties of peat and pine bark substrates by employing evaporative moisture characteristic measurements, which were originally designed for mineral soils, for soilless substrate analyses. Utilizing these evaporative measurements provide more accurate measures of substrate water potentials between -10 and -800 hPa than traditional pressure plate measurements. Soilless substrates were engineered, utilizing only three common substrate components [stabilized pine bark (Pinus taedea L.), Sphagnum peatmoss, and coconut coir fiber], via particle fractionation and fibrous additions. The engineering process yielded substrates with increased unsaturated hydraulic conductivity, pore connectivity, and more uniform pore size distributions. These substrates were tested in a greenhouse with irrigation systems designed to hold substrates at (-100 to -300 hPa) or approaching (-50 to -100 hPa) water potentials associated with drought stress. Substrate-water dynamics were monitored, as were plant morphology and drought stress indicators. It was determined that increased substrate unsaturated hydraulic conductivity within the production water potentials, allowed for increased crop growth, reduction in drought stress indicators, while producing marketable plants. Furthermore, individual plants were produced using as low as 5.3 L per plant. Increased production range substrate hydraulic conductivity was able to maintain necessary levels of air-filled porosity due to reduced irrigation volumes, while providing water for plants when needed. The substrates were able to conduct water from throughout the container volume to the plant roots for uptake when roots reduced substrate water potential. Furthermore, increased substrate hydraulic conductivity allowed plants within the substrate to continue absorbing water at much lower water potentials than those in unaltered (control) pine bark. Finally, HYDRUS models were utilized to simulate water flux through containerized substrates. These models allowed for better understanding of how individual hydraulic properties influence substrate water flux, and provided insight towards proportions of inaccessible pores, which do not maintain sufficient levels of available water. With the models, researchers will be able to simulate new substrates, and utilize model predictions to provide insight toward new substrates prior to implementing production tests. It has been determined, that increasing substrate hydraulic conductivity, which can be done with just commonly used components, water requirements for production can be reduced, to produce crops with minimal wasted water resources. Concluding, that re-engineering substrate hydrology can ameliorate production sustainability and decrease environmental impact. / Ph. D.

Planting density and genotype have close relationship with the water relations in plants. The scenario of increased occurrence of extreme weather events and the change of Eucalyptus forest plantations to high water deficit regions, led us to the three key questions of this study: (1) What is the relationship between planting density and the potential water stress? (2) The planting spacing interferes the water use efficiency (WUE), i.e. the amount of biomass produced by the amount of water transpired? (3) Can the planting density change the soil water balance (BHS)? To develop this work, we settled a field trial in Mogi Guacu, SP, in February 2012. We planted four genetic material (Eucalyptus grandis x E.urophylla1 {Urograndis1}, Eucalyptus grandis x E.urophylla2, E.urophylla and E.grandis x E.camaldulensis {Grancam}) with different levels of tolerance to drought and four planting spacings (3.4, 7.0, 10.5 and 16.9 m2 plant-1, which correspond to densities of 2,949 , 1,424 and 1,028 and 591 plants ha-1). In Chapter 1, we evaluated the leaf water potential (representing potential water stress) of the four clones for 1 year, between 1.5 and 2.5 years. Regardless of the genetic material, the higher the wood productivity, the greater the leaf water potential. The denser planting (2,949 plants ha-1) stands generated 39% more wood, however, water stress potential reached up to 33% higher than the least dense planting (591 plants ha-1). In the second chapter, during the same period, we evaluated the efficiency of water use, which did not vary according to the change of planting density, but showed differences between genotypes with US 2.3, 2.2 and 1, 5 g L-1 to Urograndis, Urophylla and Grancam, respectively, at a density of 1,424 plants ha-1. Finally, the third chapter evaluated for two years, between 1.7 and 3.7 years, transpiration (T), soil evaporation (Es) and canopy interception (Ei), which together made up evapotranspiration (ET). Subtraction of precipitation (P) per ET resulted in soil water balance (SWB). The SWB was positive or near zero for the two clones evaluated (Urograndis1 and Grancam) when planting density was less than or equal to 1,028 trees ha-1. In the denser planting, the balance was -25%. These studies show that: a higher wood growth results in a higher potential drought stress, generating a clear trade-off between production and survival of trees. However, the detailed study of genetic materials fall under that there are increasing opportunities in water use efficiency, though without the increase in water use, bringing a greater share of water in the watershed scale. Finally, plantations above 1,028 ha-1 trees resulted in a negative soil water balance of -25% at the peak of growth. Together, this study reveals that spacing associated with genotypes can serve as tools in the search for balance between timber production and conservation of natural resources. / A densidade de plantio e o genótipo possuem estreita relação com as relações hídricas nas plantas. Sob um cenário de maior ocorrência de eventos climáticos extremos e do avanço dos plantios florestais de eucalipto para regiões de elevado déficit hídrico, elaboramos três perguntas-chave para esse estudo: (1) Qual a relação entre a densidade de plantio e o potencial estresse hídrico? (2) O espaçamento de plantio interfere na eficiência do uso da água (EUA), i.e., na quantidade de biomassa produzida pela quantidade de água transpirada? (3) Pode a densidade de plantio alterar o balanço hídrico do solo (BHS)? Para responder a essas questões, instalou-se um ensaio de campo em Mogi Guacu, SP, em fevereiro de 2012. Foram plantados quatro materiais genéticos (Eucalyptus grandis x E.urophylla1 {Urograndis1}, Eucalyptus grandis x E.urophylla2, E.urophylla e E.grandis x E.camaldulensis {Grancam}) com distintos níveis de tolerância à seca e quatro espaçamentos de plantio (3,4, 7,0, 10,5 e 16,9 m2 planta-1, que correspondem às densidades de 2.949, 1.424 e 1.028 e 591 plantas ha-1). No capítulo 1, avaliou-se o potencial hídrico foliar (representando o potencial estresse hídrico) dos quatro clones durante 1 ano, entre 1,5 e 2,5 anos. Independentemente do material genético, quanto maior a produtividade madeireira atingida, maior o potencial hídrico foliar. Os plantios mais adensados (2.949 plantas ha-1) geraram povoamentos 39% mais produtivos, no entanto, o potencial estresse hídrico chegou a atingir 33% acima do plantio menos adensado (591 plantas ha-1). No segundo capítulo, durante o mesmo período, avaliou-se a eficiência do uso da água, que não variou conforme a mudança de densidade de plantio, mas apresentou diferença entre os genótipos, com EUA de 2,3, 2,2 e 1,5 g L-1 para os clones Urograndis, Urophylla e Grancam, respectivamente, na densidade de 1.424 plantas ha-1. Por fim, o terceiro capítulo avaliou durante dois anos, entre 1,7 e 3,7 anos, a transpiração (T), evaporação do solo (Es) e interceptação de água pela copa (Ei), que somados compunham e evapotranspiração (ET). A subtração da precipitação (P) da ET resultou no balanço hídrico do solo (BHS). O BHS foi positivo ou próximo de zero para os dois clones avaliados (Urograndis1 e Grancam) quando a densidade de plantio foi inferior ou igual a 1.028 árvores ha-1. No plantio mais adensado, o balanço foi de -25%. Estes estudos demonstram que: a maior produtividade madeireira acarreta em maior potencial estresse hídrico, gerando um claro dilema entre a produção e a sobrevivência dos plantios. No entanto, o estudo detalhado dos materiais genéticos releva que há possibilidades de incremento na eficiência do uso da água sem que ocorra o aumento no uso da água, trazendo um maior compartilhamento da água na escala da microbacia. Por fim, plantios acima de 1.028 árvores ha-1 resultaram em um balanço hídrico do solo negativo médio de -25% no pico do crescimento. Em conjunto, o presente trabalho releva que o espaçamento associado a materiais genéticos específicos, podem servir como ferramenta na busca pelo equilíbrio entre a produção madeireira e a conservação de recursos naturais.

Planting density and genotype have close relationship with the water relations in plants. The scenario of increased occurrence of extreme weather events and the change of Eucalyptus forest plantations to high water deficit regions, led us to the three key questions of this study: (1) What is the relationship between planting density and the potential water stress? (2) The planting spacing interferes the water use efficiency (WUE), i.e. the amount of biomass produced by the amount of water transpired? (3) Can the planting density change the soil water balance (BHS)? To develop this work, we settled a field trial in Mogi Guacu, SP, in February 2012. We planted four genetic material (Eucalyptus grandis x E.urophylla1 {Urograndis1}, Eucalyptus grandis x E.urophylla2, E.urophylla and E.grandis x E.camaldulensis {Grancam}) with different levels of tolerance to drought and four planting spacings (3.4, 7.0, 10.5 and 16.9 m2 plant-1, which correspond to densities of 2,949 , 1,424 and 1,028 and 591 plants ha-1). In Chapter 1, we evaluated the leaf water potential (representing potential water stress) of the four clones for 1 year, between 1.5 and 2.5 years. Regardless of the genetic material, the higher the wood productivity, the greater the leaf water potential. The denser planting (2,949 plants ha-1) stands generated 39% more wood, however, water stress potential reached up to 33% higher than the least dense planting (591 plants ha-1). In the second chapter, during the same period, we evaluated the efficiency of water use, which did not vary according to the change of planting density, but showed differences between genotypes with US 2.3, 2.2 and 1, 5 g L-1 to Urograndis, Urophylla and Grancam, respectively, at a density of 1,424 plants ha-1. Finally, the third chapter evaluated for two years, between 1.7 and 3.7 years, transpiration (T), soil evaporation (Es) and canopy interception (Ei), which together made up evapotranspiration (ET). Subtraction of precipitation (P) per ET resulted in soil water balance (SWB). The SWB was positive or near zero for the two clones evaluated (Urograndis1 and Grancam) when planting density was less than or equal to 1,028 trees ha-1. In the denser planting, the balance was -25%. These studies show that: a higher wood growth results in a higher potential drought stress, generating a clear trade-off between production and survival of trees. However, the detailed study of genetic materials fall under that there are increasing opportunities in water use efficiency, though without the increase in water use, bringing a greater share of water in the watershed scale. Finally, plantations above 1,028 ha-1 trees resulted in a negative soil water balance of -25% at the peak of growth. Together, this study reveals that spacing associated with genotypes can serve as tools in the search for balance between timber production and conservation of natural resources. / A densidade de plantio e o genótipo possuem estreita relação com as relações hídricas nas plantas. Sob um cenário de maior ocorrência de eventos climáticos extremos e do avanço dos plantios florestais de eucalipto para regiões de elevado déficit hídrico, elaboramos três perguntas-chave para esse estudo: (1) Qual a relação entre a densidade de plantio e o potencial estresse hídrico? (2) O espaçamento de plantio interfere na eficiência do uso da água (EUA), i.e., na quantidade de biomassa produzida pela quantidade de água transpirada? (3) Pode a densidade de plantio alterar o balanço hídrico do solo (BHS)? Para responder a essas questões, instalou-se um ensaio de campo em Mogi Guacu, SP, em fevereiro de 2012. Foram plantados quatro materiais genéticos (Eucalyptus grandis x E.urophylla1 {Urograndis1}, Eucalyptus grandis x E.urophylla2, E.urophylla e E.grandis x E.camaldulensis {Grancam}) com distintos níveis de tolerância à seca e quatro espaçamentos de plantio (3,4, 7,0, 10,5 e 16,9 m2 planta-1, que correspondem às densidades de 2.949, 1.424 e 1.028 e 591 plantas ha-1). No capítulo 1, avaliou-se o potencial hídrico foliar (representando o potencial estresse hídrico) dos quatro clones durante 1 ano, entre 1,5 e 2,5 anos. Independentemente do material genético, quanto maior a produtividade madeireira atingida, maior o potencial hídrico foliar. Os plantios mais adensados (2.949 plantas ha-1) geraram povoamentos 39% mais produtivos, no entanto, o potencial estresse hídrico chegou a atingir 33% acima do plantio menos adensado (591 plantas ha-1). No segundo capítulo, durante o mesmo período, avaliou-se a eficiência do uso da água, que não variou conforme a mudança de densidade de plantio, mas apresentou diferença entre os genótipos, com EUA de 2,3, 2,2 e 1,5 g L-1 para os clones Urograndis, Urophylla e Grancam, respectivamente, na densidade de 1.424 plantas ha-1. Por fim, o terceiro capítulo avaliou durante dois anos, entre 1,7 e 3,7 anos, a transpiração (T), evaporação do solo (Es) e interceptação de água pela copa (Ei), que somados compunham e evapotranspiração (ET). A subtração da precipitação (P) da ET resultou no balanço hídrico do solo (BHS). O BHS foi positivo ou próximo de zero para os dois clones avaliados (Urograndis1 e Grancam) quando a densidade de plantio foi inferior ou igual a 1.028 árvores ha-1. No plantio mais adensado, o balanço foi de -25%. Estes estudos demonstram que: a maior produtividade madeireira acarreta em maior potencial estresse hídrico, gerando um claro dilema entre a produção e a sobrevivência dos plantios. No entanto, o estudo detalhado dos materiais genéticos releva que há possibilidades de incremento na eficiência do uso da água sem que ocorra o aumento no uso da água, trazendo um maior compartilhamento da água na escala da microbacia. Por fim, plantios acima de 1.028 árvores ha-1 resultaram em um balanço hídrico do solo negativo médio de -25% no pico do crescimento. Em conjunto, o presente trabalho releva que o espaçamento associado a materiais genéticos específicos, podem servir como ferramenta na busca pelo equilíbrio entre a produção madeireira e a conservação de recursos naturais.

La germination est un processus clé qui conditionne la régénération des plantes dans leur milieu ainsi que leur distribution. Connaître les conditions thermique et hydrique qui permettent aux plantes de germer est un préalable nécessaire à l’identification des menaces qui pèsent sur elles et tout particulièrement dans un contexte de changement climatique. Les modèles en temps thermique et temps hydrique permettent de prédire la phénologie de germination sur le terrain en fonction des conditions climatiques dans l’environnement de la graine dépassant des valeurs seuil de température et de potentiel hydrique de base, Tb et Ψb (i.e. respectivement la température minimale et le potentiel hydrique minimum permettant la germination).Dans ce travail de thèse, il est donc question d’étudier l’écophysiologie de la germination à l’aide de ces modèles à deux échelles taxonomiques : (i) celle des plantes à graines et (ii) à l’échelle du genre Silene de la région PACA. Dans les deux cas le but est d’évaluer les contraintes évolutives des traits de réponse au climat de la germination ainsi que leurs liens avec les contraintes morphologiques et phénologiques des plantesLes résultats de cette thèse montrent un fort signal phylogénétique des traits de germination de la température de base et une plus grande labilité pour le potentiel hydrique de base quelle que soit l’échelle taxonomique considérée. En revanche, les liens avec les traits des plantes, tels que la masse des graines, sont plus variables et dépendent à la fois de l’origine biogéographique et de la longévité des espèces. / Germination is a key process in plant reproduction, a critical and irreversible phase conditioning the regeneration and distribution of plants. Understanding how temperature and water act on germination, is major step prior to identify risks plants may undergo under warming climate. Thermal time and hydrotime modelling of germination are useful tools to predict germination in the field as a function of climatic conditions above threshold value of temperature and water potential (respectively base temperature, Tb, and base water potential, Ψb) in a seed’s environment. This PhD thesis aimed at studying germination ecophysiology at two contrasted taxonomic scales: (i) for all seed plants and (ii) at the restricted level of the genus Silene in the Provence Alpes Côte d’Azur region. In both cases the objective was to evaluate evolutionary implications of the germination traits, Tb and Ψb and their link with plant morphological and phenological constraints. This work is structured in three parts : (I) Temperature but not moisture response of germination shows phylogenetic contraints while both interact with seed mass and life span ; (II) Germination ecophysiology in the Silene genus : thermal time and hydrotime models ; (III) Comparative ecology of Silene germination : relation with plant traits and climate.The mains results of this work show strong evidences of phylogenetic signal in base temperature and greater lability for base water potential at both taxonomic scales. The links with plant traits such as seed mass depend on biogeographical origins and life span.

No description available.

Submitted by (lucia.rodrigues@ufrpe.br) on 2016-08-31T10:53:10Z No. of bitstreams: 1 Maria Alice Vasconcelos da Silva (1).pdf: 762537 bytes, checksum: c100c2c556639aa3d440082da1ef7bb5 (MD5) / Made available in DSpace on 2016-08-31T10:53:10Z (GMT). No. of bitstreams: 1 Maria Alice Vasconcelos da Silva (1).pdf: 762537 bytes, checksum: c100c2c556639aa3d440082da1ef7bb5 (MD5) Previous issue date: 2007-08-30 / Coordenação de Aperfeiçoamento de Pessoal de Nível Superior - CAPES / This work aimed to study the effect of water deficit on gas exchange, leaf water potential, dry matter production, and some biochemical aspects of Schinus terebinthifolius Raddi. young plants. A research project was developed, under greenhouse conditions, at the Laboratório de Fisiologia Vegetal, Departamento of Biologia of Universidade Rural de Pernambuco between November, 2005 to February, 2006. Seedlings with 3 month-old and sexually propagated were cultivated in containers containing 5.5 kg of soil. The entirely randomized experimental design was used, with four water treatments (100%, 75%, 50% and 25% to field capacity-FC), with four replicates. Plants under 25% FC were re-watered to 100% FC once after stomatal closure. After 15 days of acclimation period have started the water treatments. The experimental period lasted for 74 days. Transpiration (E), diffusive resistance (Rs), leaf temperature (Tfol), air temperature (Tar), relative humidity of the air (UR), photosynthetically active radiation (PAR), and vapor pressure deficit (VPD) were evaluated at midday each seven days. At the end of the experimental period, leaf water potential (Yf) was measured at midday. Leaves (LDM), stems (SDM), roots (RDM), and total dry masses (TDM), root to shoot ratio (R/Sh), and leaves (LBA), stems (SBA) and roots biomass allocation (RBA) were determined. In addition, carbohydrates, free proline, soluble protein and free amino acids contents were analyzed. In plants under 25% field capacity, stomatal closure was observed after 11 days of water treatments. At the time plants were re-watered to 100% FC. After 24 h plants re-watered recovered the stomatal aperture, which remained open until the end of the experimental period. Water deficit decreased the leaf water potential (Yf) in plants grown at 25% FC (-2.2 MPa) when compared with the 100% FC treatment (-1.1 MPa). Plants grown under 75% FC producted higher LDM, SDM and RDM than the other treatments. Differences among treatments to biomass allocation were not observed, but there was a tendency to plants grown under 25% of FC to increase more biomass allocation than the other treatments. The water stress reduced carbohydrates contents and increased soluble protein and amino acids. However, differences to proline content were not verified among water treatments. These results suggest that this species is tolerate to low humidity levels in the soil and that the level of 75% of FC is the best to cultivate it in the initial fase of development. / Com o objetivo de estudar os efeitos do déficit hídrico sobre as trocas gasosas, o potencial hídrico foliar, a produção de matéria seca e alguns aspectos bioquímicos de plantas jovens de Schinus terebinthifolius Raddi, foi desenvolvido um trabalho em casa de vegetação do Laboratório de Fisiologia Vegetal do Departamento de Biologia da Universidade Federal Rural de Pernambuco, no período de novembro de 2005 a fevereiro de 2006. Utilizaram-se mudas com três meses de idade, propagadas sexuadamente, as quais foram transferidas para vasos de polietileno contendo 5,5 kg de solo. Adotou-se um delineamento experimental inteiramente casualizado, representado por quatro tratamentos hídricos (100% da Capacidade de pote; 75% CP; 50% CP; 25% CP) com quatro repetições. Após 15 dias sob aclimatação, procedeu-se o início dos tratamentos hídricos. Durante o período experimental foram efetuadas medições das trocas gasosas do vapor d’água às 12 horas em intervalos de 7 dias. Avaliou-se a transpiração (E), a resistência difusiva (Rs), a temperatura foliar (Tf), a temperatura do ar (Tar), a umidade relativa do ar (UR), a radiação fotossinteticamente ativa (RFA) e o déficit de pressão de vapor (DPV). No final do período experimental foi mensurado o potencial de água da folha (Yf) às 12 horas e determinado o peso da matéria seca das folhas (MSF), dos caules (MSC), das raízes (MSR), a matéria seca total (MST), a relação raiz/parte aérea (R/Pa) e a alocação de biomassa para as folhas (ABF), caules (ABC) e para as raízes (ABR). Além disso, foram analisados os teores de carboidratos, de prolina livre, proteínas solúveis e aminoácidos livres. O fechamento estomático ocorreu em plantas submetidas a 25% CP, aos 11 dias após a diferenciação dos tratamentos hídricos quando as plantas foram reirrigadas para 100% CP. Após 24 horas houve recuperação da abertura estomática mantendo-se até o final do experimento. O déficit hídrico reduziu o potencial hídrico foliar (Yf) nas plantas do tratamento estresse moderado (–2,2 MPa) quando comparado com o controle (-1,1 MPa). As plantas do tratamento 75% CP se destacaram em relação aos demais tratamentos, por produzirem mais matéria seca para as folhas (MSF), caule (MSC) e raízes (MSR). Com relação à alocação de biomassa, não houve diferença significativa entre os tratamentos, porém houve uma tendência do tratamento 25% CP alocar mais biomassa para do que os demais tratamentos. Em relação aos solutos orgânicos, o déficit hídrico provocou reduções nos teores de carboidratos e aumento no teor de proteínas e aminoácidos, não havendo diferença entre os tratamentos para os teores de prolina. Os resultados sugerem que a aroeira é tolerante a baixos níveis de umidade no solo e que o nível de 75%CP é o mais indicado para o cultivo desta espécie na fase de muda.

Made available in DSpace on 2016-12-23T14:37:33Z (GMT). No. of bitstreams: 1 Dissertacao Maria Christina Junger.pdf: 2116125 bytes, checksum: a838fb12301a6580f6dc47358feed2c7 (MD5) Previous issue date: 2006-02-24 / The objective of this work was to evaluate the influence of the soil humidity in the field capacity in the tensions of 0,006 MPa (FC1), 0,010 MPa (FC2) and 0,033 MPa (FC3) and of different levels of water deficits (WD 0%, WD 33% and WD 67%) in the initial growth of the coffee plant conilon and in the leaf water potential measured in the anti-morning, in a Red-Yellow Oxisol (OR) and Red-Yellow Ultisol (URY). The experiment was let vegetation home, being cultivated the plants in vases of 12 liters during 255 days. The adopted experimental design was randomized entirely, mounted in outline of subdivided portions, with three repetitions for each soil. The growth evaluations were achieved each 60 days and the analyzed data by the surface technique of answering. The tenor of soil humidity in the field capacity varies with the adopted tension in its determination. The growth of the coffee plant conilon in WD 0% was higher to the obtained in the water deficits of 33% and 67% of OR and URY. The largest growth of the culture was observed in FC2 of OR and in FC1 of URY. The smallest growth was obtained in the water deficits of the certain field capacity in the tension of 0,033 MPa (FC3) of OR and URY, what unfeasible its adoption in the estimate of the irrigation sheet, being used the camera of pressure of Richards. The x leaf water potential anti-morning (Ψam) showed to be a good indicator of the degree of hydration of the plants. The largest hydration to foliate was observed in WD 0%, being in CC2 for OR (Ψam = -0,17 MPa), being the water kept by the soil to a potential matric (Ψm) of -0,010 MPa and in CC1 for URY (Ψam = -0,33 MPa), which Ψm was the -0,006 MPa. To smallest hydration happened in WD 67% and in the FC3, also for OR (Ψam = -0,68 MPa) as for URY (Ψam = -1,3 MPa), being the water kept of Ψm of -0,20 MPa, for both soils. In WD 33% and WD 67% in the levels of the capacity of field of OR and URY, they were verified a reduction in the values leaf area, height and diameter of the stem of the plants. The accumulation of total dry matter and leaf water potential anti-morning observed in OR were superior to the of URY, in all of the levels of the field capacity and water deficits, resulting in the larger initial growth of the coffee plant conilon in this soil. / O objetivo deste trabalho foi avaliar a influência da umidade do solo na capacidade de campo determinada nas tensões de 0,006 MPa (CC1), 0,010 MPa (CC2) e 0,033 MPa (CC3) e de diferentes níveis de déficits hídricos (DH 0%, DH 33% e DH 67%), no crescimento inicial do cafeeiro conilon e no potencial hídrico foliar medido na antemanhã, em um Latossolo Vermelho-Amarelo (LV) e Argissolo Vermelho-Amarelo (PVA). O experimento foi conduzido em casa de vegetação, cultivando-se as plantas em vasos de 12 litros durante 255 dias. O delineamento experimental adotado foi inteiramente casualizado, distribuído em esquema de parcelas subdivididas, com três repetições para cada solo. As avaliações de crescimento foram realizadas a cada 60 dias e os dados analisados pela técnica de superfície de resposta. O teor de umidade do solo na capacidade de campo varia com a tensão adotada em sua determinação. O crescimento do cafeeiro conilon em DH 0% foi superior aos obtidos nos déficits hídricos de 33% e 67% do LV e do PVA. O maior crescimento da cultura foi observado na CC2 do LV e na CC1 do PVA. O menor crescimento foi obtido nos déficits hídricos da capacidade de campo determinada na tensão de 0,003 MPa (CC3) do LV e do PVA, o que inviabiliza a sua viii adoção na estimativa da lâmina de irrigação, utilizando-se a câmara de pressão de Richards. O potencial hídrico foliar antemanhã (Ψam) mostrou-se bom indicador do grau de hidratação das plantas. A maior hidratação foliar foi observada em DH 0%, sendo para o LV na CC2 (Ψam= -0,17 MPa), estando a água retida pelo solo a um potencial matricial (Ψm) de -0,010 MPa, e para o PVA na CC1 (Ψam = -0,33 MPa), cujo Ψm foi de -0,006 MPa. A menor hidratação ocorreu em DH 67% na CC3 tanto para o LV (Ψam = -0,68 MPa) como para o PVA (Ψam = -1,30 MPa), estando a água retida a um Ψm de -0,20 MPa, para ambos os solos. Em DH 33% e DH 67% nos níveis de capacidade de campo do LV e do PVA, foram verificadas reduções nos valores da área foliar, altura e diâmetro do caule das plantas. O acúmulo de matéria seca total e potencial hídrico foliar antemanhã observados no LV foram superiores aos do PVA, em todos os níveis de capacidade de campo e déficits hídricos, resultando em maior crescimento inicial do cafeeiro conilon, neste solo.

Submitted by Gabriela Lopes (gmachadolopesufpel@gmail.com) on 2018-08-13T17:46:02Z No. of bitstreams: 1 Cópia revisada ledemar-Luciano PDF.pdf: 1720131 bytes, checksum: 693af5179fe3089038ef47e6746002c4 (MD5) / Approved for entry into archive by Aline Batista (alinehb.ufpel@gmail.com) on 2018-08-16T18:55:29Z (GMT) No. of bitstreams: 1 Cópia revisada ledemar-Luciano PDF.pdf: 1720131 bytes, checksum: 693af5179fe3089038ef47e6746002c4 (MD5) / Made available in DSpace on 2018-08-16T18:55:29Z (GMT). No. of bitstreams: 1 Cópia revisada ledemar-Luciano PDF.pdf: 1720131 bytes, checksum: 693af5179fe3089038ef47e6746002c4 (MD5) Previous issue date: 2017-09-29 / A produção de pêssego ocupa destaque entre as frutíferas de clima temperado no Brasil, sendo o Estado do Rio Grande do Sul responsável por 65 % da produção. Para obter elevada produtividade com frutos de qualidade, o pessegueiro requer adequado suprimento de água durante a primavera e o verão. Neste período, é frequente a ocorrência de déficit hídrico e a irrigação pode promover aumento de rendimento e qualidade dos frutos. Os objetivos deste trabalho foram: avaliar a resposta do pessegueiro à irrigação, quanto ao estado hídrico das plantas e a produtividade e qualidade dos frutos; determinar o manejo de água no solo mais adequado para a cultura do pessegueiro; e avaliar a influência da textura do solo no manejo da água. O estudo foi realizado em um pomar de pessegueiro comercial, cv Esmeralda, localizado no município de Morro Redondo - RS, durante as safras 2014/15, 2015/16 e 2016/17. Foram demarcadas duas áreas homogêneas em função da classe textural do solo, sendo classificadas como Franco Arenosa e Franco Argilo Arenosa. As plantas foram irrigadas por sistema de irrigação localizada por gotejamento. Os resultados mostraram que: a irrigação na fase de crescimento de fruto não influenciou a produtividade nem o tamanho dos frutos; a irrigação na fase de pós-colheita aumentou o crescimento vegetativo na safra seguinte mas não afetou a produção de frutos; os pessegueiros da área do pomar com solo franco arenoso produziram frutos maiores do que os da área com solo franco argilo arenoso; o manejo da irrigação baseado no potencial de água no ramo gera maior consumo de água, seguido pelo manejo baseado no teor de água no solo e, por último, o manejo baseado no clima / The production of peach stands out among the fruits of temperate climate in Brazil, being the State of Rio Grande do Sul (RS) responsible for 65% of the production. To achieve high productivity with quality fruits, the peach tree requires adequate water supply during spring and summer. During period, water deficit is frequent and irrigation can promote yield increase and fruit quality. The objectives of this study were to evaluate the peach response to irrigation, as the water status of plants and productivity and fruit quality; to determine the soil water management most appropriate for the peach tree; and to evaluate the influence of soil texture on water management. The study was carried out in a commercial peach orchard, cv Esmeralda, located in the municipality of Morro Redondo - RS, during the harvests of 2014/15, 2015/16 and 2016/17. Two homogeneous areas were demarcated according to the textural class of the soil, being classified as Sandy Loam and Sandy Clay Loam. The plants were irrigated by a drip irrigation system. The results showed that: irrigation in the fruit growth phase did not influence fruit productivity nor fruit size; post-harvest irrigation increased vegetative growth in the next crop but did not affect fruit production; the peach orchard area with sandy loam soil produced larger fruit than the area with sandy loam clay soil; the management of irrigation based on the water potential in the branch generates greater water consumption, followed by management based on the water content in the soil and, finally, the management based on the climate.

Introducing effective irrigation management in arid and semi-arid regions, like most areas of South Africa, is an indispensable way of maximising crop yield and enhancing productivity of scarce freshwater resources. Holistic improvements in agricultural water management could be realised through integrating the knowledge of crop-specific water requirements. In order to develop effective irrigation schedules for rose-scented geranium (Pelargonium capitatum x P. radens), greenhouse and field experiments were conducted at the Hatfield Experimental Farm of the University of Pretoria, Pretoria, South Africa, from 28 October 2004 to 2006. Results from 20, 40, 60 and 80% maximum allowable depletion (MAD) levels of the plant available soil water (ASW) indicated that plant roots extracted most of the soil water from the top 40 cm soil layer, independent of the treatment. Both essential oil yield and fresh herbage mass responded positively to high soil water content. Increasing the MAD level to 60% and higher resulted in a significant reduction in herbage mass and essential oil yields. An increase in the degree of water stress apparently increased the essential oil concentration (percentage oil on fresh herbage mass basis), but its contribution to total essential oil yield (kg/ha oil) was limited. There was no significant relationship between MAD level and essential oil composition. For water saving without a significant reduction in essential oil yield of rose-scented geranium, a MAD of 40% of ASW is proposed. Response of rose-scented geranium to a one-month irrigation withholding period in the second or third month of regrowth cycles showed that herbage mass and oil yield were positively related. Herbage yield was significantly reduced when the water stress period was imposed during the third or fourth month of regrowth. A remarkable essential oil yield loss was observed only when the plants were stressed during the fourth month of regrowth. Essential oil content (% oil on fresh herbage mass basis) was higher in stressed plants, especially when stressed late, but oil yield dropped due to lower herbage mass. The relationship between essential oil composition and irrigation treatments was not consistent. Water-use efficiency was not significantly affected by withholding irrigation in the second or in the third month of regrowth. With a marginal oil yield loss, about 330 to 460 m3 of water per hectare per regrowth cycle could be saved by withholding irrigation during the third month of regrowth. The overall results highlighted that in water-scarce regions withholding irrigation during either the second or the third month of regrowth in rose-scented geranium could save water that could be used by other sectors of society. In greenhouse pot experiments, rose-scented geranium was grown under different irrigation frequencies, in two growth media. Irrigation was withheld on 50% of the plants (in each plot) for the week prior to harvesting. Herbage and essential oil yields were better in the sandy clay soil than in silica sand. Essential oil content (% oil on fresh herbage mass basis) apparently increased with a decrease in irrigation frequency. Both herbage and total essential oil yields positively responded to frequent irrigation. A one-week stress period prior to harvesting significantly increased essential oil content and total essential oil yield. Hence, the highest essential oil yield was obtained from a combination of high irrigation frequency and a one-week irrigation-withholding period. In the irrigation frequency treatments, citronellol and citronellyl formate contents tended to increase with an increase in the stress level, but the reverse was true for geraniol and geranyl formate. Leaf physiological data were recorded during the terminal one-week water stress in the glasshouse pot trial. Upon rewatering, stomatal conductance (Gs) and transpiration rate (Rt) were significantly lower in the less often irrigated than in the more often irrigated treatments, while leaf water potential (yw) and relative water content (RWC) were the same for all plants, indicating that water stress had an after-effect on Gs and Rt. At the end of the stress period, Gs, Rt, yw and RWC were lower in the plants from the more often irrigated than from the less often irrigated treatments. Irrespective of irrigation treatment, one type of non-glandular and two types (different in shape and size) of glandular trichomes were observed. In water stressed-conditions, stomata and trichome densities increased, while the total number of stomata and trichomes per leaf appeared to remain more or less the same. Water stress conditions resulted in stomatal closure. / Thesis (PhD)--University of Pretoria, 2009. / Plant Production and Soil Science / unrestricted

L’objectif de ce travail était de caractériser la variabilité saisonnière des échanges gazeux des arbres de la canopée en forêt tropicale humide guyanaise confrontés à des saisons sèches.L’étude s’est orientée sur la mesure des flux de carbone et d’eau au cours des saisons sèches dans deux habitats contrastés du point de vue hydrique, afin de préciser leur sensibilité et réponse à la sècheresse. Nos résultats montrent qu’une proportion non négligeable d’arbres ne subit pas de sécheresse marquée en saison sèche, malgré la forte diminution de la teneur en eau du sol en surface. Nous faisons l’hypothèse que ces arbres possèdent alors des racines en profondeur qui leur permettent d’accéder aux horizons qui restent humides malgré la faible pluviométrie. Durant les longues saisons sèches, nous observons une diminution de l’assimilation nette de CO2 foliaire, de l’efflux de CO2 des troncs ou de la densité de flux de sève, et dans une moindre mesure de la respiration foliaire. Cette diminution concerne un nombre plus important d’arbres, quand l’intensité de la sécheresse est plus forte (2008 par rapport à 2007). Néanmoins, de grandes différences de réponse à la sècheresse du sol ont été observées, suggérant des sensibilités et des mécanismes de réponse différents entre ces arbres. En habitat de bas-fond, nous montrons une plus faible diminution des flux carbonés et hydriques en saison sèche, suggérant un accès pour ces arbres aux horizons humides, proches de la nappe phréatique. Par ailleurs, nos résultats suggèrent pour certains arbres un effet négatif des conditions d’anoxie sur ces flux en saison des pluies.Si l’accentuation de l’intensité des saisons sèches en forêt tropicale humide Amazonienne se confirme, comme suggérée par les modèles climatiques, ce travail suggère des modifications rapides de la composition spécifique des forêts, au profit des espèces plus résistantes aux contraintes hydriques / The aim of this work was to characterize the seasonal variations in leaf and trunk gas exchange of tropical rainforest canopy trees exposed to dry seasons. This study focused on measuring gas exchange (CO2 and H2O) at the leaf and trunk level during dry seasons in a Terra firme forest and in a seasonally flooded forest in order to specify their sensitivity and response to drought.Our results showed that part of the studied trees do not encounter a large reduction in soil water content during dry seasons, suggesting that they display deep rooting systems.During long dry periods, we recorded a decrease in leaf photosynthesis, trunk CO2 efflux or sap flow density, and foliar respiration to a lesser extent, for a majority of the trees. Nevertheless, large differences among trees in their response to these conditions were observed, suggesting distinct sensitivities and response to soil drought among trees. Furthermore, these variations were greatest when soil drought was highest (2008 as compared to 2007).In seasonally flooded forest, the decrease in gas exchange was less, suggesting that these trees do have access to wet layers during the dry season, close to the groundwater. However, during wet seasons, we observed a negative effect of anoxia for some trees, whereas others did not display any response, suggesting large differences in tolerance to anoxia among trees abundant in these seasonally flooded forests.We conclude that would seasonal soil droughts increase over the next decades, large vegetation changes might occur because of the large differences among trees in their functional response to soil drought conditions