As famílias rurais do semiárido vivem sob constante vulnerabilidade climática, cujas atividades agropecuárias são comprometidas pela instabilidade hídrica, pela produção em solos empobrecidos e também pela demanda de altos investimentos na modernização dos seus sistemas produtivos. A consequência é um povo marginalizado, pobre, sem acesso a alimentação em quantidade e qualidade suficientes, desencadeando na migração para grandes centros ou ainda, a exploração e degradação dos recursos da Caatinga na tentativa de desenvolver suas atividades e assim permanecer no campo. Diante a problemática da seca, muitas estratégias de convivência com o semiárido são promovidas, as quais favorecem o acesso à água e a inclusão social. No entanto, o cenário atual enfatiza a necessidade de medidas mais eficientes para o fortalecimento da agricultura familiar, que devem ser condizentes à realidade do agricultor e harmoniosas com o meio ambiente. Portanto, para elucidar questões sobre a realidade de agricultores familiares do semiárido e gerar informações como subsídio a atuação de agentes externos, o presente trabalho compreendeu as vulnerabilidades dos meios de vida de agricultores familiares. Bem como, a importância e o impacto dos recursos (água, produção e área consolidada) dos meios de vida de agricultores familiares. Foram realizadas entrevistas com 23 famílias distribuídas em municípios da Bacia do Jacuípe e aplicados quatros métodos multivariados, por meio da (i) análise de agrupamentos, (ii) análise de componentes principais, (iii) análise de fatores e (iv) análise de seleção das variáveis. Os resultados apontaram para a produção que aqueles com maior número de matrizes (vacas em lactação ou caprinos para carne) diversificam suas rendas com a venda de galinhas e ovos e possuem RL com entrada de animais. Enquanto aquelas com propriedades entre 0-20 ha trabalham, somente, com a produção de hortaliças, cuja fonte de renda é o próprio negócio. Famílias com propriedades entre 20-66 ha criam caprinos, não possuem APP e não utilizam equipamentos via associações ou empréstimos. Quanto as famílias com propriedades entre 66-80 ha, embora criem caprinos, sua comercialização não é a principal fonte de renda. Assim, concluiu-se que os meios de vida das famílias rurais do semiárido apresentam maior vulnerabilidade nos seguintes recursos: financeiro (devido ao baixo retorno econômico de suas atividades e à comercialização de seus produtos, bem como às dificuldades de acesso ao crédito) e social (falta de conhecimentos técnicos resultando em práticas agropecuárias defasadas e insustentáveis, desencadeando uma má utilização dos recursos locais). O acesso aos programas sociais disponíveis e a participação em associações ou cooperativas são fundamentais para viabilizar as estratégias de convivência com o semiárido. A gestão da água (acesso e bom uso do recurso) e a aplicação dos conhecimentos tradicionais favorecem a segurança alimentar das famílias rurais. As principais estratégias de convivência com o semiárido focam no acesso a água e em alternativas para suprir a falta de alimento para o animal. O tamanho da propriedade e de produção impactam a conservação da caatinga, assim como, o tamanho da propriedade influencia no foco de produção agropecuário. Por fim, o uso eficiente da água depende de tecnologias e boas práticas que permitam o seu melhor aproveitamento. / Countryside families who lives in the semi-arid region are under constant climate vulnerability, whose agricultural activities are compromised by water instability, production in impoverished soils and by the demand for high investments in the modernization of their productive systems. The consequence is a marginalized, poor people, without access to food in sufficient quantity and quality, triggering the migration to big centers or the exploitation and degradation of Caatinga resources in attempt to develop their activities and thus remain in rural areas. Faced with drought problem, many strategies for living with the semi-arid are promoted, which favor access to water and social inclusion. However, the current scenario emphasizes the need for more efficient alternatives to strengthen family farming, which must be applicable to reality of farmers and harmonious with environment. Based on the assumption that more financial resources favor the development of family agriculture, but also the awareness of use and better exploitation of local resources available in their lives, the present work understood importance and use of resources of the livelihoods (human, Social, physical, financial and natural) through the methodology Sustainable Livelihoods. interviews were conducted with 23 families included on a program called Adapta Sertão, selected with a focus on production and size of the property, distributed in municipalities of the Jacuípe Basin. To verify the impact of family farmer livelihoods, 20 factors were generated based on 99 observed variables and four multivariate methods were applied, through (i) cluster analysis, (ii) principal component analysis, (iii) analysis of factors and (iv) analysis of selection of variables. The results showed that, based on the production focus, most of the families work with milk production, and there is a direct relationship between a higher production of animals and, consequently, a lower presence of APP. Families with higher numbers of animals (lactating cows or goats for meat) are those that diversify their family income through the sale of chickens and eggs, but who have RL with animals. Families with properties between 0-20 ha are those that produce only vegetables and have their own business as main source of income (they do not work with raising goats and selling milk). Families with properties between 20-66 ha, have no APP and do not use equipment via associations or loans. However, they are those that work with the creation of goats. Regarding families with properties between 66-80 ha, although they raise goats, their commercialization is not the main source of income. Thus, it was concluded that the guarantee of food security of countryside families who lives in the semi-arid region are vulnerable in the following resources: financial (due to the low economic return of their activities and the commercialization of their products, as well as the difficulties of access to credit) and (Lack of technical knowledge resulting in lagging and unsustainable agricultural practices, triggering misuse of local resources). Access to available social programs and participation in associations or cooperatives are fundamental to enable the strategies to coexist with the semi-arid region.

Die semiaride Steppe der Inneren Mongolei (China) ist ein gefährdetes Ökosystem. Der Wandel vom traditionellen nomadischen Lebensstil hin zur konventionellen Landwirtschaft überlastet die Steppe und führt zu Degradierung und Desertifikation. Besonders die intensive Beweidung belastet die weiten Grasflächen und mindert deren natürliches Potential Kohlen-stoff (C) im Boden zu speichern. Um den Einfluss unterschiedlicher Beweidungsintensitäten auf die semiaride Steppe zu untersuchen, wurden im Rahmen des Projektes Matter fluxes in grasslands of Inner Mongolia as influenced by stocking rate (MAGIM) das Einzugsgebiet des Xilin Flusses in der Inneren Mongolei von 2004 bis 2009 untersucht. Dafür wurden u. a. meteorologische und Eddykovarianz-Messungen an definierten Standorten durchgeführt. Ziel dieser Messungen war es, die Unterschiede im Energiehaushalt und den Kohlendioxid- und Wasserflüssen (CO2- und H2O-Flüsse) für die dominanten Steppenarten und unter verschiedenen Beweidungsintensitäten zu erfassen. Die Schließung der Energiebilanz ergab eine Schließungslücke von 10 – 30% in Abhängigkeit der meteorologischen Bedingungen, wobei die Lücke unter feuchten Bedingungen kleiner ist. Die gemessenen CO2- und H2O-Flüsse sind klein im Vergleich zu Grasländern in den gemäßigten Zonen und reagieren sensitiv auf Veränderungen der Einflussfaktoren. Dabei ist die Evapotranspiration (ET) eng an den eingehenden Niederschlag (P) gekoppelt und über längere Zeiträume wie ein Jahr entspricht ET dem P (ET: 185,7 mm a-1 bis 242 mm a-1; P: 138 mm a-1 bis 332 mm a-1). Die Jahressummen für den Nettoökosystemaustausch (NEE) reichen von -10,7 g C m-2 a-1 (2005) bis -67,5 g C m-2 a-1 (2007) für die unbeweidete Steppe und charakterisieren diese als eine leichte Nettosenke für atmosphärisches CO2. Grundsätzlich zeigt die unbeweidete Steppe eine höherer C-Sequestrierung (maximale C-Sequestrierung im Mittel -0,06 g C m-2 s-1) als die beweidete Steppe (maximale C-Sequestrierung im Mittel -0,02 g C m-2 s-1). Die Messergebnisse zeigen, dass die Steppe unter trockenen Verhältnissen zur CO2-Quelle wird, unter erhöhten Niederschlagsbedingungen zur CO2-Senke und die Beweidung die C-Sequestrierung des Ökosystems unter beiden Bedingungen einschränkt. Im Vergleich der beiden Steppenarten (Leymus chinensis und Stipa grandis) konnte für Leymus chinensis eine höhere Trockentoleranz beobachtet werden. Diese führt zu einer höheren C-Sequestrierung unter trockeneren Verhältnissen. Unabhängig von der Steppenart sind die wichtigsten Einflüsse auf das Ökosystem die Bodenfeuchte, die vom eingehenden P abhängt, die Temperatur (T) und die Beweidung. Diese Faktoren können dabei nicht unabhängig voneinander betrachtet werden. Der Einfluss durch die Beweidung beeinflusst das Ökosystem nachhaltig, wobei die Intensität und die Dauer (Jahre) der Beweidung entscheidend sind, da nicht nur die oberirdische Biomasse reduziert wird, sondern gleichzeitig die Bodeneigenschaften. Um die Sensitivität auf den CO2- und H2O-Austausch der semiariden Steppe über die Messungen hinaus abzuschätzen, wurden Simulationen mit den Modellen BROOK90 und DAILYDAYCENT (DDC) durchgeführt. Beide Modelle konnten gut an die Bedingungen der semiariden Steppe angepasst werden, wobei die Übereinstimmung zwischen der gemessenen und modellierten ET für BROOK90 besser war (r2 = 0,7) als für DDC (r2= 0,34). Beide Modelle konnten gut die Dynamik der ET-Messungen wiedergeben. Die Sensitivitätsanalyse hat gezeigt, dass die Beziehung zwischen P und ET entscheidend für das Ökosystem ist und sich Änderungen in der T nur zum Ende und Beginn der Vegetationsperiode auf den Wasseraustausch auswirken. DDC konnte sehr gut den gemessenen CO2-Austausch simulieren. Die Ergebnisse zeigen die Sensitivität gegenüber den klimatischen Faktoren T, P und der Beweidung. Die CO2-Flüsse werden durch hohe Beweidungsintensitäten so stark minimiert, dass andere Einflussfaktoren dahinter zurücktreten. Bei leichten Beweidungsintensitäten wirkt sich dagegen besonders der P auf die Austauschprozesse aus. Die DDC-Ergebnisse zeigen, dass unter den derzeitigen Bedingungen der bodenorganische Kohlenstoff (SOC) verringert wird, also C aus dem Boden freigesetzt wird. Auch unter unbeweideten Verhältnissen steigt der SOC nicht wieder auf das Ausgangsniveau (von vor der Beweidung) an. Die Ergebnisse zeigten, dass die C-Sequestrierung der Steppe nur erhöht werden kann, wenn der P steigt, die T in einem Optimumbereich (+/- 2°C) bleibt und die Beweidung minimiert wird. Die Messungen und Modellergebnisse zeigen, dass der Niederschlag der limitierende Faktor der semiariden Steppe ist. P bestimmt die Bodenfeuchte, diese wiederum beeinflusst das Pflanzenwachstum und somit den CO2- und H2O-Austausch der Pflanzen. Die Beweidung strapaziert das Ökosystem und reduziert dadurch die CO2- und H2O-Flüsse und verändert die Bodeneigenschaften nachhaltig. Unabhängig von der klimatischen Entwicklung, ist die derzeitige überwiegend hohe Beweidungsintensität der Steppe eine Belastung für das Ökosystem und schränkt das Pflanzenwachstum langfristig ein, was u. a. die Desertifikation begünstigt. / Semiarid grasslands in Inner Mongolia (China) are degrading. The change from the traditional Nomadic lifestyle to conventional agriculture stresses the semiarid grasslands and increases desertification. In particular, intense grazing of the semiarid grasslands reduces their potential of storing carbon (C) in the soil. In the project Matter fluxes in grasslands of Inner Mongolia as influenced by stocking rate (MAGIM) a team of scientists researched the catchment area of the Xilin River to investigate impacts of different grazing intensities on semiarid grasslands. Meteorological and eddy covariance measurements took place from 2004 to 2009. The aim of the measurements was to examine the energy balance and the exchange of the carbon dioxide (CO2) and water (H2O) fluxes of the dominant grasslands in Inner Mongolia under different grazing intensities. The energy balance could be closed by 70 – 90% depending on the driving factors. The energy balance shows a smaller gap for moist conditions. The CO2 und H2O fluxes in the study area are much smaller than in temperate grasslands and show a high sensitivity towards the driving factors. Evapotranspiration (ET) is closely connected to the precipitation (P) and over longer periods of a year or more, ET nearly matches P (ET: 185.7 mm a-1 to 242 mm a-1; P: 138 mm a-1 to 332 mm a-1). The annual net ecosystem exchange (NEE) of ungrazed grassland ranges from -10.7 g C m-2 a-1 (2005) to -67.5 g C m-2 a-1 (2007), which makes the grassland a small CO2-sink. Overall, ungrazed grassland shows higher C sequestration (averaged maximum -0.06 g C m-2 s-1) than grazed grassland (averaged maximum -0.02 g C m-2 s-1). The measurements show the semiarid grassland as a CO2-source under dry conditions and as a CO2-sink under moist conditions, while grazing decreases the C sequestration for both climatic conditions. A comparison of the two dominant steppe types (Leymus chinensis and Stipa grandis) showed a higher tolerance for Leymus chinensis under dry conditions, which resulted in higher C sequestration for this vegetation. Besides the steppe type, the main driving factors are P, temperature (T) and grazing. These factors can not only be considered in isolation, but cross correlation needs to get considered as well. Grazing affects the sustainability of the ecosystem, with an increasing impact due to grazing intensity and duration (years). The impact of grazing influences the vegetation directly and shows indirect impacts for the soil properties. Simulations with the models BROOK90 and DAILYDAYCENT (DDC) enable a sensitivity analysis of CO2 and H2O fluxes of the semiarid grassland. Both models performed well, but BROOK90 showed a better fit to observed ET (r2 = 0.7) than DDC (r2= 0.34). Both models simulated the dynamics of the measured ET well. The sensitivity analysis showed a close relationship between P und ET and a smaller impact on ET due to a change in T. DDC performs well in the simulation of CO2 exchange dynamics of the semiarid grassland. The results show for high grazing intensities a decreasing influence of the other driving factors. A change in P has an influence on CO2 and H2O fluxes under low grazing intensities. The results also show a decrease in soil organic carbon (SOC) as grazing intensity increases (under current climatic conditions). An increase in SOC could only be achieved under an increase in P, an optimum T and low grazing intensities. The measurements and results of the simulations indentify P as the main driving factor controlling the CO2 and H2O fluxes in the semiarid grassland. P influences the soil moisture and this influences plant growth, which governs the CO2 and H2O exchange of the vegetation. Grazing decreases the CO2 and H2O exchange and affects the soil properties in the long term. Besides climate change, the current high grazing intensities of the semiarid grassland have a negative impact on the ecosystem, decreasing plant growth and increasing desertification.

Thesis (M.Sc. Agriculture (Pasture Science)) -- University of Limpopo, 2020 / Bush encroachment is a major problem in arid and semi-arid savannas characterized by a grass layer interspersed with a shrub stratum. Land cover change as a result of rapid proliferation of woody species in previously open rangelands alters herbaceous species and impacts soil properties. So far, little is known about the threshold at which woody plant density and cover affects herbaceous cover and the underlying mechanisms driving bush encroachment in arid and semi-arid rangelands are still debated. The objectives of this dissertation were to (1) to assess woody species composition and structure along an encroachment gradient and to explore the relationship between woody vegetation and herbaceous vegetation. (2) To determine the effect of increasing tree density and cover on grass species richness, diversity, evenness and selected soil nutrients in a bush encroached rangeland. In order to address these objectives, a semi-arid rangeland was demarcated into three encroachment gradients spanning from open to intermediate and intensive. Within each encroachment gradient six plots of 10 m x 10 m were randomly selected, whereby woody and herbaceous vegetation were assessed and soil properties determined. A discernible increase in woody species diversity and evenness was found along the transition from open to intensive bush encroached rangeland. Leguminous woody species Vachellia spp. and Dichrostachys cinerea were dominant along the bush encroachment gradient. Tree height was found to be positively correlated with long crown diameter (LCD) and short crown diameter (SCD). Furthermore, increasing tree density resulted in a 53% decline in grass species richness (GR). A decline in GR mirrored an increase in the composition of the decreaser species Panicum maximum (90%). Increasing woody plant density and cover also increased macro-nutrients; total carbon, nitrogen, phosphorus, exchangeable calcium and magnesium by 21%-159% in the shallow rangeland soils. Such quantitative information will assist rangeland managers to better understand the effects of varying bush encroachment intensities on herbaceous species composition, richness and soil properties in semi-arid savanna rangelands.

MSCAGR (Plant Production) / Department of Plant Production / Chickpea (Cicer arietinum L.) is an important grain legume in the world, ranking second after soybean (Glycine max L.). It accounts for a substantial proportion of human dietary nitrogen intake and plays a crucial role in food security in developing countries. Chickpea can grow in areas with low rainfall and poor soils, and thus may be an important food security crop for smallholder resource-poor farmers in the semi-arid tropics such as the dry environments of the Limpopo and Mpumalanga Provinces of South Africa. Preliminary studies showed the huge potential of chickpea production in these environments. However, no suitable genotypes have been identified and recommended for different agro-ecological zones of Limpopo and Mpumalanga Provinces. Therefore, the objective of this study was to evaluate the performance, and hence, identify the genotypes that are adapted/suitable to the contrasting agro-ecological conditions of Limpopo and Mpumalanga Provinces for production. Field experiments were conducted in the winter cropping seasons of 2016 and 2017 at Thohoyandou (University of Venda experimental station), Syferkuil (University of Limpopo experimental station) and Nelspruit (University of Mpumalanga experimental station). Ten desi chickpea genotypes were sown in a completely randomized block design replicated three times on 10 May 2016 and 10 April 2017 (Thohoyandou), 13 May 2016 and 11 April 2017 (Syferkuil) and 03 May 2016 and 24 May 2017 (Nelspruit). Plant growth characteristics were assessed by determining plant height, crop phenology, number of primary and secondary branches, and canopy cover. Yield and yield components were assessed at harvest after physiological maturity. Carbon dioxide exchange rates (CER) was determined at different growth stages using the InfraRed Gas Analyzer (IRGA). Chlorophyll content (CC) and intercepted radiation were determined weekly using the chlorophyll content meter (CCM-200 PLUS, Opti-Science, Tyngsboro, Massachusetts), and the AccuPAR, LP-80 ceptometer (Deacon Devices Ltd., Pullman, USA), respectively. Genotypes did not vary in CC at Thohoyandou in all seasons, but CC increased with stages of growth. Genotypes varied in the proportion of intercepted radiation (IR) at all measurement dates in Thohoyandou during the 2016 and 2017 growing seasons. The proportion of IR increased with growth stage, reached a peak and declined with plant age. Genotype affected photosynthesis and intercellular CO2 concentration (Ci) but did not have any significant effect on stomatal conductance (gs), transpiration (T) and Leaf Vapour Pressure Deficit (VPDL) during the 2016 season in Thohoyandou. In contrast, genotype did not affect photosynthesis, Ci, gs, T and VPDL in the 2017 season in Thohoyandou. There was no variation among genotypes on number of primary and secondary branches in Thohoyandou in both seasons. Genotypes showed no variation in plant height in the 2016 season in Thohoyandou agro-ecological condition. However, genotypes showed significant variation in plant height at 14, 70 and 84 days after emergence (DAE) in the 2017 cropping season. Moreover, genotypes showed significant variations in days to 50% flowering in Thohoyandou during the 2016 season, but showed no variations in days to 50% emergence and 75% physiological maturity. Genotypes showed no variations in days to 50% emergence, 50% flowering, 50% podding and 75% physiological maturity in the 2017 season in all locations. Genotypes showed significant variation in grain yield in Syferkuil agro-ecological condition, but showed no significant variations on all the other studied traits, while genotypes varied in 100 seed weight (SW) in Thohoyandou, but did not show any variations on the other studied traits during the 2016 season. Moreover, genotypes did not vary for all studied traits in Nelspruit during the 2016 season. The 2016 genotype and environment (G X E) interaction results showed no significant variations. However, results showed G X E interactions during the 2017 growing season suggesting that genotypes responded to environmental variation in a different way. Syferkuil had the greatest grain yield (2811 kg ha-1 and 3122 kg ha-1) in both the 2016 and 2017 growing seasons respectively, as compared to Thohoyandou and Nelspruit. These preliminary findings show that the studied genotypes responded differently in contrasting agro-ecological regions of Limpopo and Mpumalanga Provinces and that Syferkuil might be the best environment for chickpea production in this region due to its cooler temperatures. Of the genotypes evaluated the most promising genotypes are ICCV8101, ICCV3203 and ICCV4110 in these regions in terms of grain yield. / NRF

No description available.

Thesis (MScAgric)--Stellenbosch University, 2012. / ENGLISH ABSTRACT: Soils of semi-arid regions generally have low organic matter contents, primarily attributed to prevailing climatic conditions. Yet, the spekboom thicket, located in the semi-arid region of the Eastern Cape (South Africa) has been distinguished to accumulate large amounts of soil carbon. To further understand this remarkable accumulation, a detailed investigation was carried out to evaluate the distribution, speciation and stability of the soil carbon from directly beneath spekboom (Portulacaria afra) and other “nonspekboom” vegetation within the intact thicket, and from adjacent, degraded (overgrazed), open thicket sites. In the first experimental chapter, the distribution of organic and inorganic C, as well as general soil properties (pH, EC, exchangeable and water soluble cations, hydrophobicity, water stable aggregates) were investigated in the intact (spekboom and nonspekboom) and degraded (open) thicket soils. There were no significant differences in the C content (organic or inorganic) between the spekboom and nonspekboom sites in the intact thicket. Soil organic carbon (SOC) content however was greatly influenced by thicket degradation, whereas, inorganic C remained unaffected. Mean organic C (0-50 cm) ranged from 19-34, 22-62, and 19-58 g C kg-1 for open, spekboom, and nonspekboom sites, respectively. Whereas, mean inorganic C ranged from 2-9 g C kg-1 irrespective of sites, representing 4-22 % of total soil C. However, no significant differences were detected between degraded and intact sites for all (total, organic and inorganic) C stocks, attributed to variation in bulk density. Spekboom soils contained significantly higher concentrations of exchangeable and water soluble Mg, Na, and K, and consequently had higher pH and EC compared to the other sites. Soils tended to be hydrophobic especially at shallower depths in the intact thicket irrespective of vegetation type, whereas soils from the adjacent open sites were not significantly hydrophobic. Macro-aggregates were considerably more stable under intact sites compared to open sites. The second experimental chapter investigated the effects of degradation and vegetation type on the stability and structural chemistry of SOC. This involved partitioning the soil organic matter into particulate and mineral-bound (stable) fractions, and then examining the relationships between the stable organic C fraction and various soil properties as an attempt to elucidate the stabilization mechanism(s). Particulate organic C ranged from 7.0, 9.3, and 14.4 g C kg-1 for open, spekboom, and nonspekboom respectively; representing 22-34 % of total SOC. Stable (mineral-bound) organic C accounted for the largest fraction ca. 60-66 % of total SOC; 28.0 and 26.2 g C kg-1 for spekboom and non-spekboom respectively, versus 17.2 g C kg-1 for open sites. It was concluded that SOC stability was influenced by the inherent residue quality (recalcitrance) rather than soil properties, attributed to the aliphatic (lipids and waxes) and highly aromatic nature of the spekboom litter substrate and particulate OM. These research findings are of fundamental significance in understanding soil organic matter stabilization in semi-arid environments. / AFRIKAANSE OPSOMMING: Gronde van semi–ariede streke het oor die algemeen 'n lae organiese materiaalinhoud, wat hoofsaaklik aan die heersende klimaatstoestande toegeskryf kan word. Tog, het die spekboomruigtes, geleë in die semi-ariede streek van die Oos-Kaap (Suid Afrika), onderskeidelik groot hoeveelhede grondkoolstof geakkumuleer. Om hierdie merkwaardige akkumulasie verder te verstaan, was 'n gedetailleerde ondersoek uitgevoer om die verspreiding, spesiasie en stabiliteit van die grondkoolstof direk onder spekboom (Portulacaria afra) en ander “nie-spekboom” plantegroei binne die intakte ruigte en van die aangrensende gedegradeer (oorbeweide), oop gras areas te evalueer. In die eerste eksperimentele hoofstuk, is die verspreiding van organiese en anorganiese C, sowel as algemene grondeienskappe (pH, uitruilbare en wateroplosbare katione, hidrofobisiteit, water-stabiele aggregate) was in die intakte (spekboom en nie-spekboom) en degradeerde (oop) ruigtes ondersoek. Daar was geen betekenisvolle verskille in die C-inhoud (organies of anorganies) tussen die spekboom en nie-spekboom gronde in die intakte ruigtes gevind nie. Grond organiese koolstof (GOK) inhoud is grootliks deur die ruigte se agteruitgang beïnvloed, maar anorganiese C-voorrade was egter nie beïnvloed nie. Die gemiddelde organiese C-inhoud (0-50 cm) het van 19-34, 22-62 en 19-58 g C kg-1 onderskeidelik vir 'n oop, spekboom, en nie-spekboom areas gewissel. Die anorganiese C-inhoude het vanaf 2-9 g C kg-1 gewissel, ongeag van ligging, wat 4-22 % van die totale grond C uit maak. Daar is egter geen beduidende verskille tussen vervalle en heel terreine vir almal (totaal, organiese en anorganiese) C aandele opgespoor, toegeskryf word aan die variasie in die massadigtheid. Spekboom gronde het beduidende hoër konsentrasies van uitruilbare en wateroplosbare Mg, Na, en K waardes bevat. Dit het ook hoër pH en EC, in vergelyking met die ander areas gehad. Gronde was geneig om hidrofobies te wees, veral op vlakker dieptes in die intakte ruigte, ongeag van die plantegroei, terwyl die gronde van die aangrensende oop areas nie beduidend hidrofobies was nie. Makro grond aggregate was aansienlik meer stabiel onder intakte ruigtes as in die oop areas. Die tweede eksperimentele hoofstuk het die gevolge van die weiding-geïnduseerde degradasie en tipe plantegroei op die stabiliteit en strukturele chemie van GOK ondersoek. Dit het die skeiding van die grond organiese materiaal in die vrye en mineraalgebonde (stabiele) fraksies behels. Daarna is die verhoudings tussen die stabiele organiese C fraksie en verskeie grondeienskappe ondersoek om die stabiliseringmeganisme(s) uit te lig. Die chemiese aard van die blare, plante oorblyfsels, fyn en minerale gebinde organiese C is met behulp van spektroskopie ondersoek. Vrye organiese C voorraad het van 7.0, 9.3, en 14.4 g C kg-1 vir oop, spekboom, en nie-spekboom onderskeidelik gewissel, wat ongeveer 23-34% van die totale GOK verteenwoordig. Stabiele (minerale gebind) organiese C-voorrade is vir die grootste fraksie ca. 60-66% van die totale GOK verantwoordelik. Dit was 28.0 en 26.2 g C kg-1 onderskeidelik vir spekboom en nie-spekboom, teenoor 17.2 g C kg-1 vir 'n oop area. Die mineraalgebonde GOK het geen noemenswaardige korrelasies met die ondersoekte grondeienskappe getoon nie. Dus is tot die gevolgtrekking gekom dat GOK stabilisering eerder deur die plante oorblyfsel se chemiese kwaliteit beïnvloed word. Strukturele chemiese karakterisering (13C CP-MAS KMR) van die spekboom afval en vrye C fraksie het gewys dat weerspannigheid die mees prominente meganisme van koolstof stabilisering van organiese koolstof in die gronde is. Dit word aan die alifatiese (lipiede en wasse) en sterk aromatiese aard van die spekboom substrate toegeskryf. Hierdie ondersoek het tot die fundamentele kennis van grond organiese materiaalstabilisering in 'n semi-ariede omgewings bygedra.

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Afin de mieux comprendre et évaluer l'impact du changement climatique sur les stocks de carbone organique du sol (COS) et les flux de carbone, et en particulier la respiration hétérotrophe du sol (RS), il est nécessaire d'étudier la sensibilité de la RS à la température. Plusieurs études sur les facteurs contrôlant la dépendance de la RS à la température ont été faites antérieurement et montrent que la sensibilité de la RS à la température diminue avec la température. Ces études ont suggéré que cette diminution de sensibilité de la RS à la température était liée à la modification de la disponibilité en substrat. D'autres études ont suggéré que cette diminution est liée à l'adaptation de la communauté microbienne aux températures élevées. La sensibilité de la RS à la température est plus particulièrement critique dans les régions semi-arides, comme le Nord Ouest de la Tunisie où le stock de COS est faible. Il est nécessaire de connaître l'effet de la disponibilité en substrat sur la sensibilité de la RS à la température. Dans cette étude, les échantillons de sol ont été incubés pendant 28 jours après une période de 28 jours de pré-incubation. Les pré-incubations et incubations ont été réalisées à 20, 30, 40 et 50°C. Pour tester l'effet de la disponibilité en substrat sur la sensibilité de la RS à la température, du glucose a été ajouté au sol au début de la période d'incubation. L'analyse des résultats a montré que les températures élevées de pré-incubation réduisent la sensibilité de la RS à la température d'incubation. L'addition de glucose réduit l'effet de températures élevées de pré-incubation sur la réponse de la RS. Il apparaît ainsi que la diminution de la sensibilité de la RS après un mois de pré-incubation aux fortes températures est due à la diminution de la disponibilité en substrat. Elle semble aussi liée à une diminution de la biomasse microbienne. Puisque, le sol utilisé pour cette étude est un Cambi sol Calco-magnésimorphe, une deuxième expérimentation a été réalisée afin de déterminer la part de CO2 provenant des carbonates et la part de CO2 provenant du COS. Cette étude a été réalisée par des mesures des signatures isotopiques (δ13C) du COS, des carbonates et du CO2 émis. Après 28 jours d'incubation, 23±9% de CO2 provient des carbonates. Cette contribution est faible par rapport à la teneur initiale élevée de C-CaCO3 dans le sol (4,3%) et est indépendante de la température d'incubation. Cette étude a montré que la réduction de la sensibilité de la RS aux fortes températures est surtout liée à une réduction de la disponibilité en substrat organique et de la biomasse microbienne aux fortes températures. / To better understand and assess the impact of climate change on the stocks of soil organic carbon (SOC) and carbon fluxes, and particularly heterotrophic soil respiration (SR), it is necessary to study the sensitivity of SR to temperature. Several studies have been achieved to improve the understanding of factors controlling the temperature dependence of SR and showed that the temperature sensitivity of SR decreases with temperature. These studies suggested that this decrease in temperature sensitivity of SR was related to change in substrate availability. Other studies presented microbial adaptation to warmed conditions. The temperature sensitivity of SR is especially critical in semi-arid regions, such as North West Tunisia, where the SOC stock is low. It is necessary to know the influence of substrate availability on the sensitivity of SR to temperature. In this study, soil samples were incubated for 28 days after a 28-day pre-incubation per iod. Pre-incubation and incubation were carried out at 20, 30, 40 and 50°C. To test the substrate availability effect on the temperature sensitivity of SR, glucose was added to soil at the beginning of the incubation period. Results showed that the highest pre-incubation temperature reduced the temperature sensitivity of SR during the subsequent incubation period. Glucose addition reduced the effect of high pre-incubation temperature on SR response. Thus, it appears that the observed decrease in SR sensitivity to temperature after one month pre-incubation at high temperature was due to a reduce in substrate availability and to a decrease in microbial biomass. Since the soil used in this study is a Calcari-Leptic Cambisol, a second experiment was also performed to determine the amount of CO2 from carbonates and the amount of CO2 from SOC. This study was carried out by measurements of the isotopic signatures (δ13C) of SOC, carbonates and emitted CO2. After 28 days of inc ubation, 23±9% of CO2 came from carbonates. This contribution was low compared to the high initial C-CaCO3 content in soil (4.3%), and it was independent to the incubation temperature. This study showed that reduce in the sensitivity of SR to high temperatures was probably due to a reduction in the substrate availability and to a decrease in microbial biomass.

A Caatinga, bioma exclusivamente brasileiro, inserido no clima semiárido nordestino, apresenta xerófitas com alta resistência aos períodos de seca. Estas plantas associam-se a micro-organismos que também se encontram bem adaptados, desenvolvendo mecanismos de proteção celular contra o estresse hídrico, assim como proteção vegetal contra os efeitos negativos da dessecação. O presente estudo buscou compreender as bactérias associadas às cactáceas da Caatinga, analisando a estrutura das comunidades bacterianas de solo e da rizosfera de Cereus jamacaru durante a alteração do período chuvoso para o de seca, identificando os grupos dominantes e discutindo algumas funções que possibilitem a manutenção da interação solo-cacto-micro-organismo durante o período de seca. Além disso, buscou selecionar bactérias tolerantes à seca e que fossem capazes de promover crescimento de plantas sob estresse hídrico. Amostras foram coletadas ao longo da Caatinga, em cinco estados: BA, CE, PI, PB e RN totalizando cinco pontos. Com o uso de metodologias independentes de cultivo, foi possível observar que o período de amostragem (chuvoso/seca) foi o principal responsável pela alteração na estrutura das comunidades bacterianas. Os filos Proteobacteria e Bacteroidetes foram abundantes durante o período chuvoso e os filos Actinobacteria e o gênero Bacillus abundantes durante o período de seca. Com o uso de metodologias dependentes de cultivo, foram isoladas com bastante frequência linhagens pertencentes ao gênero Bacillus, capazes de crescer em meio com reduzida atividade de água e com alguns mecanismos de proteção contra a dessecação, como a produção de exopolissacarídeos e biofilme. Além disso, várias linhagens apresentaram mecanismos de promoção de crescimento de plantas diretos e/ou indiretos, como produção de fitohormônio, disponibilização de P por meio de solubilização, fixação de nitrogênio, redução dos efeitos negativos do estresse causados por etileno, produção de celulase e amônia. Uma linhagem de Bacillus sp. foi capaz de promover crescimento de milho sob estresse hídrico, incrementando alguns parâmetros vegetais analisados. São discutidos o uso de consórcio bacteriano entre duas linhagens, além dos mecanismos que os micro-organismos dispõem para tolerar condições ambientais adversas e ainda as funções que estes micro-organismos podem ter na proteção vegetal contra a dessecação. / Caatinga, a Brazilian unique biome, inserted in the semi-arid climate of Brazilian northeast, presents xerophytes with high resistance to drought periods. These plants are found in association with well-adapted microorganisms that have evolved some cellular protection mechanisms against water stress, as well as plant protection against the negative effects of desiccation. This work aimed to study the bacteria associated to some Caatinga cacti, with respect to the structure of bacterial communities of bulk soil and rhizosphere of Cereus jamacaru during the modification of rainy season to dry season, identifying the dominant groups and discussing some functions that enable the soil-cactus-microorganism interaction maintenance during drought. Besides, we searched for drought-tolerant bacteria able to promote plant growth under water stress. Samples were collected along the Caatinga biome in five states: BA, CE, PI, PB, and RN in a total of five points. With unculturable techniques, it was possible to observe that the sampling season (rainy/dry) was the main driver for the modification of bacterial communities\' structure. Proteobacteria and Bacteroidetes phyla were the most abundant during the rainy season while phylum Actinobacteria and Bacillus group were the most abundant during the dry season. With culturable techniques, it was observed a high frequency of strains belonging to genus Bacillus that were able to grow in medium at reduced water activity and displaying some mechanisms of desiccation protection such as the production of exopolysaccharides and biofilm. Furthermore, several strains showed mechanisms of direct and/or indirect plant growth promotion, like the production of fitohormone, availability of P through solubilization, nitrogen fixation, reduction of negative effects caused by stress-induced ethylene, production of cellulase and ammonia. One strain of Bacillus sp. was able to promote maize growth under water stress, increasing some of the analyzed plant parameters. The use of bacterial consortium between two strains, as well as mechanisms displayed by microorganisms under adverse environmental conditions and their functions in plant protection against desiccation are also discussed.

A Caatinga é um ecossistema brasileiro análogo as savanas africanas apresentando escassez de chuvas e temperaturas altas. O mocó apresenta, importantes adaptações ao microambiente dos afloramentos rochosos. Esse roedor caviomorfo, abandonou o hábito pastador comum a outros roedores cavíneos, como preá e a capivara, pela capacidade de escalar árvores e se alimentar de folhas e frutos. Alongou o período de gestação e adotou o cuidado paterno. Interessados em entender de que forma a comunicação acústica teria se ajustado ao ambiente isolado dos rochedos da caatinga, gravamos e analisamos as emissões sonoras dos mocós. Foram 90 dias de trabalho de campo nas Fazendas Tamanduá e São Francisco, na cidade de Patos, Paraíba. Capturamos 13 animais (6 machos e 7 fêmeas) e fizemos registros em áudio e vídeo em três situações: 1) pareamentos em caixa teste, nas condições macho x macho, macho x fêmea e fêmea x fêmea, 2) animais em grupo em cativeiro, e 3) animais em vida livre. Encontramos um repertório de 11 sinais sonoros, registrados em 3 categorias amplas de comportamento: (1) Exploração/Forrageamento: Có de contato, Estalido, Chorinho e Drrr; (2) Alerta: Assobio de alarme, Drrr e Silvo; (3) Interação Agonística: Ganido, Grito, Ronco, Arfar, Assobio de alarme e o Baterdedentes. O repertório mostrouse mais rico do que o de outros caviomorfos, como o preá. Discutimos esse resultado em relação ao tipo de vida social da espécie em comparação com a de outros caviníneos e à vida nos rochedos da caatinga. Também sugerimos que o Assobio de alarme seja um comportamento compartilhado entre o mocó e outras espécies de roedores 10 de rochedos. Há uma perspectiva de continuidade da pesquisa em busca de uma maior compreensão da função biológica desse sinal e da riqueza desse repertório acústico / The environment of Brazilian Caatinga ecosystem is similar to African Savannah with low level of rain and high temperature. The Moco shows important adaptation at the microenvironment of rock outcrops. This caviomorph rodent abandoned grazing habit, commom at others Caviinae species such as the Cavy and the Capybara for the capacity of climbing trees feeding of leaves and fruits. It also lengthened the gestation period and adopted paternal care. Interested in understanding how acoustic communication would have adjusted to the isolated environment of Caatinga rock piles, we recorded and analyzed the signals songs of Moco. Past through 90 days in field at Fazenda Tamanduá and Sítio São Francisco located at Patos city Paraiba State in Brazil. We captured 13 animals (6 males and 7 females), acquired audio and video of animals in three different situations: 1) paired in tests boxes under conditions: male x male, female x male and female x female; 2) captivity group and 3) Living free. We found a repertoire with 11 acoustic signals registered in 3 broad behavioral categories: (1) Exploration/ Foraging: Contact call, Co, Clicking (Estalido), Whine (Chorinho) and Drrr call, (2) Warning: Alarm whistle, Drrr call and Silvo, (3) Agonistic Interaction: yelp (Ganido), scream (Grito), grunt (Ronco), a breathless like sound (Arfar), Alarm Whistle and ToothChatter. This repertoire showed more rich that other caviomorph as a cavy. eu escreveria esse parágrafo dessa forma: This repertoire seemed better than other caviomorph as a Cavy. We discussed those results comparing the social life of species with social life of others Caviinae and the life at the rock piles of Caatinga. We also suggested that the Alarm whistle is shared between the 12 Moco and others rock rodents. There is a perspective to continue this research looking for a better comprehension of the biologic function of this signal and acoustic repertoire richness