METHODS OF ASSESSING THE SPORICIDAL EFFICIENCY OF AN ULTRA-HIGH-TEMPERATURE MILK STERILIZING PLANT. III. LABORATORY DETERMINATIONS OF THE HEAT RESISTANCE OF SPORES OF BACILLUS SUBTILIS IN WATER AND IN MILK

SUMMARY: Thermal death curves for spores of Bacillus subtilis 786 have been determined in water and in milk. Generally a non-logarithmic order of death was observed. Numbers of survivors were lower in milk than in water, suggesting that there may be inhibitory factors in UHT sterilized milk which affect the germination and/or subsequent growth of heated spores.
The thermal death curves for spores suspended in milk yielded Q₁₀ values of about 30 in the range 110–120°. This is higher than the figures previously reported in the literature for R. subtilis spores. Spores of a number of strains of B. subtilis were compared with strain 786 and all gave high Q₁₀ values.
The results obtained in this work have been used to predict the destruction of spores at higher temperatures in a UHT plant (Burton et al. 1958). The calculated values agree well with the results obtained in the plant by Franklin et al. (1958).     

The Effect of Light on the Osmotic Behaviour of the Plumular Hook

Exposure to light brings about a fall in the plasmolyticallydetermined osmotic pressure of the cells of the plumular hookof Vicia to about half the ‘dark’ value. Analysesand conductivity measurements show that light causes a smallrise in osmotically active solutes, which is confirmed by cryoscopicmeasurements. The contradiction lies in an abnormally high ‘dark’plasmolytic value, which is not attributable to entry of theplasmolysing solute; it is tentatively suggested that this isan imbibition phenomenon, and that the effect of light is todecrease the affinity for water by promoting a rise in molecularweight of the cell proteins.     

Seasonal variations in the carbohydrate content of bracken

The amounts of dry matter, mobile carbohydrate and reserve carbohydrate have been determined in bracken fronds and buds, frond-bearing rhizomes and storage rhizomes over a period of 13 months. Dry matter and reserve carbohydrate levels are closely linked, especially in the rhizomes, falling from May to the beginning of July and rising until complete frond death at the end of September; but variations occur between frond-bearing and storage rhizomes. The carbohydrate reserve of frond-bearing rhizome is rapidly exhausted by the developing fronds and further carbohydrate is drawn from the storage rhizomes, but a concurrent fall in mobile carbohydrate suggests that the rate of conversion of reserve carbohydrate is slower than the rate of translocation to the fronds. By August, there is an accumulation of carbohydrate in the frond-bearing rhizome, which is followed by a fall in September and this again suggests low enzyme activity in the storage rhizome, but also that sink strengths in bracken are in the order (1) developing buds, (2) storage rhizome, (3) frond-bearing rhizome.
The responses of bracken to cutting and herbicide-application are discussed in relation to sink strengths and a low level of enzyme activity in the storage rhizome.     

Carbon dioxide blocks the stigma callose response following incompatible pollinations in Brassica

Abstract. Carbon dioxide is known to overcome sporophytic self-incompatibility in Brassica. Elevated CO₂ (30 mmol CO₂ mol^-1 air), supplied via a flowthrough gas system, was shown to block the formation of rejection callose in the surface stigmatic papillae of Brassica campestris var. T15 following self-pollination. Possible mechanisms by which CO₂ may affect callose formation are discussed.     

Atmospheric deposition, mass balances, and processes regulating streamwater solute concentrations in mixed-conifer catchments of the Sierra Nevada, California

Solute concentrations in atmospheric deposition and stream water were measuredfrom 1984 through 1993 to determine the fate and mobility of solutes in twogauged mixed-conifer catchments (Tharp's and Log creeks) located in theSierra Nevada, California. The two catchments contain mature forest standsdominated by Abies concolor (white fir), Sequoiadendron giganteum (giantsequoia), Abies magnifica (red fir) and Pinus lambertiana (sugar pine).Ammonium, Cl^-, Ca²⁺ and NO^- ₃were highest in concentration of the solutes measured in wet deposition;bulk deposition was highest in SO^{2- 4}, NH⁺ ₄,Cl^- and H⁺. Net retention ofH⁺, NO₃ ^-, NH₄ ⁺,SO₄ ^2- and Cl^- occurred in both catchments.Discharge was dominated by spring snowmelt with the largest export yieldsfor acid neutralizing capacity (ANC), SiO₂, andCa²⁺. Export yields of H⁺,NO₃ ^-, NH₄ ⁺ and PO₄ ^3-were relatively small (0.5 kg ha^-1 y^-1).Discharge-concentration relationships for ANC, SiO₂,Na⁺, K⁺, Ca²⁺ andMg²⁺ were inverse and their concentrations in stream waterwere primarily influenced by discharge and annual differences in the relativecontributions of snowmelt and groundwater. The mobility of these solutes iscontrolled by the rates of mineral weathering and ion exchange. The positiverelationship of SO₄ ^2- concentration with increasingdischarge suggests that atmospherically deposited SO₄ ^2-is temporarily stored and that its release is controlled by the extent of soilwater flushing.     

Splash dispersal of Coniothyrium minitans in the glasshouse

Coniothyrium minitans, a mycoparasite with biocontrol activity against Sclerotinia sclerotiorum, was found to disperse during glasshouse trials where overhead irrigation was used. Consequently, the role of water splash in dispersal of C. minitans was investigated using soil-incorporated inoculum and a range of irrigation regimes found to occur in the glasshouse. The resulting inoculum deposition over horizontal distances up to 2 m was measured. Using drops < 6 mm diameter at 680 mm h^-1, C. minitans was splash-dispersed at least 2.0 m, whereas with drops > 6 mm diameter at 30 mm h^-1 it was dispersed to only 1.75 m. Irrigation with droplets < 1mm diameter at 49 mm h^-1 failed to disperse inoculum beyond 0.5 m. The dispersal gradient produced by drops < 6 mm diameter at 680 mm h^-1 was best described mathematically by the power function, whereas irrigation with drops > 6 mm diameter at 30 mm h^- resulted in a gradient described well by power or exponential functions. The latter regime produced a significantly steeper gradient than irrigation with drops < 6 mm diameter at 680 mm h^-1. C. minitans was isolated using an Andersen air sampler at concentrations of 2839 cfu m^-3 or 22 cfu m^-3 during irrigation with drops < 6 mm diameter at 680 mm h^-1 or > 6 mm diameter at 30 mm h^-1, respectively. After irrigation, deposition of C. minitans-canying aerosol particles declined exponentially and distance from source had no effect on the amount of inoculum isolated. Conidia of C. minitans, splash-dispersed by irrigation with drops < 6 mm diameter at 680 mm h^-1 were able to infect sclerotia of S. sclerotiorum such that almost all sclerotia at 0.5 m from the inoculum source, and c. 50% of those at 2.0 m, became infected with the mycoparasite.     

Does irrigation affect leaf phenology in deciduous and evergreen trees of the savannas of northern Australia?

Abstract Soil moisture was augmented experimentally during two successive dry seasons and the intervening wet season in a humid tropical savanna in Darwin, northern Australia. Leaf phenology was monitored in four common tree species Termmalia ferdinandiana and Planchonia careya (both deciduous species), and Eucalyptus miniata and Eucalyptus tetrodonta (both evergreen species). Irrigation produced consistently significant effects in only T. ferdinandiana. In this species leaf-flush was significantly earlier, canopy decline and leaf-fall were significantly later and the attainment of full canopy was earlier in irrigated compared with non-irrigated trees. Litterfall, and the seasonal patterns of contraction and expansion of stems (a measure of stem water status or storage) were not significantly affected by irrigation in any species. Leaf longevity in the deciduous species was 6–8 months; some eucalypt leaves lived for approximately 1 year, but none lived longer than 18 months. Irrigation had relatively little effect on leaf longevity. While variation in soil moisture is a potentially important cue to both leaf-fall and leaf-flush, stem water status and climatic factors such as vapour pressure deficit may also be important climatic cues to phenological behaviour.