Land use and stream nitrogen concentrations in agricultural watersheds along the central coast of California.

In coastal California nitrogen (N) in runoff from urban and agricultural land is suspected to impair surface water quality of creeks and rivers that discharge into the Monterey Bay Sanctuary. However, quantitative data on the impacts of land use activities on water quality are largely limited to unpublished reports and do not estimate N loading. We report on spatial and temporal patterns of N concentrations for several coastal creeks and rivers in central California. During the 2001 water year, we estimated that the Pajaro River at Chittenden exported 302.4 Mg of total N. Nitrate-N concentrations were typically <1 mg N l(-1) in grazing lands, oak woodlands, and forests, but increased to a range of 1 to 20 mg N l(-1) as surface waters passed through agricultural lands. Very high concentrations of nitrate (in excess of 80 mg N l(-1)) were found in selected agricultural ditches that received drainage from tiles (buried perforated pipes). Nitrate concentrations in these ditches remained high throughout the winter and spring, indicating nitrate was not being flushed out of the soil profile. We believe unused N fertilizer has accumulated in the shallow groundwater through many cropping cycles. Results are being used to organize landowners, resource managers, and growers to develop voluntary monitoring and water quality protection plans.

Effects of salinity on severity of infection by Phytophthora parasitica Dast., ion concentrations and growth of tomato, Lycopersicon esculentum Mill.

The response of tomato (Lycopersictm esculentum Mill., cv. UC82B) to salinity, alone and in combination with Phytophthora parasitica Dast. (a fungal pathogen causing root rot) was investigated in a field study. Three salinity regimes were established: 1) a low salinity control, 2 medium salinity, where 75 mm total salts (NaCl and CaCU in a 4:1 molar ratio of Na:Ca) were added to the irrigation water to give an electrical conductivity (EC) of approximately 8 dS m-1 , and 3) high salinity, where ISO mM total salts (4:1 molar ratio of Na: Ca) gave an EC of approximately 16 dS m-1 . Half of the plots were inoculated with P. parasitica. and the remainder were treated with a selective fungicide to inhibit the pathogen. Soil salinity markedly increased the incidence of Phytophthora root rot in both years of the study. The combination of salinity and enhanced disease severity led to significant reductions in fresh fruit yields, fruit size and, to a lesser extent, total above ground biomass. Fruit size was affected to the greatest extent and showed a strong interaction between the effects of disease and salinity, suggesting that the import of water by fruit was more sensitive than dry matter production to the combination of these stresses. Net root growth (0-50 cm depth) was greatly reduced (by 40-50%) in the presence of salinity, whereas P. parasitica had no discernable effect even when more than 50% of the root system showed severe root rot lesions. In spite of the reduced root system, leaf water potential was not affected by disease in the 1989 growing season. During the fruit-fill period in 1988, however, leaf water potential was more negative in inoculated plots. A marked degree of leaf ion homeostasis was maintained even under high salt and root rot stress. Excessive build up of Cl or Na concentrations in the leaves did not contribute substantially to the observed reductions in plant growth and yield. The results suggest that a reduced root growth rate or an enhanced root death rate may be at least partially responsible for the increased disease severity at high salinity.

Variation in [75 Se]selenate uptake and partitioning among tomato cultivars and wild species.

Eight Lycopersicon esculentum cultivars and six wild taxa from four Lycopersicon species were tested for their ability to transport and distribute Se under low and high sulphate salinity conditions. Plants were exposed to [75 Se]selenate for 1 h. Significant variation was observed in both morphological and transport characteristics that control the short-term uptake and accumulation of selenate in tomato species. Among L. esculentum cultivars under low salinity, selenate uptake ranged from 126-184 pmol g f. wt root-1 h-1 and shoot 75 Se concentrations ranged from 40-66 pmol g f. wt shoot-1 . Shoot accumulation was affected by both specific root weight (SRW, root fresh weight/total plant fresh weight) and uptake of the cultivar. Distribution of tracer between root accumulation and transport to the shoot, expressed on a root weight basis, was similar in all cultivars. High sulphate salinity reduced uptake to around 22 pmol g f. wt root-1 h-1 in all cultivars and only small differences in shoot 75 Se concentration (7.4-10.5 pmol g f. wt shoot-1 ) were observed, indicating that root uptake rate was the primary determinant of shoot 75 Se concentration under these conditions. In the low-salinity treatment wild accessions showed a wider range of uptake rates (52-190 pmol g f. wt root-1 h-1 ) and shoot Se concentrations (12-79 pmol g f. wt shoot-1 ) than the cultivars. High sulphate salinity had a less inhibitory effect on Se uptake in the wild taxa than in the cultivars, with uptake rates of 18-63 pmol g f. wt root-1 h-1 and shoot concentrations of 7-28 pmol g f. wt shoot-1 measured. Differences in uptake, partitioning and SRW all contributed to the variation in shoot 75 Se uptake in these taxa at both salinity levels. One cultivar (UC82B) was tested under high chloride salinity. Uptake was reduced by 40% relative to the low salt control, compared with the 87% reduction observed under high sulphate salinity. The apparent inhibition in the presence of chloride salinity could be explained by the 40% reduction in selenate activity calculated for this solution relative to the control. Reduced selenate activity was insufficient to account entirely for the reduced uptake observed in this taxon under high sulphate salinity. In contrast, after allowing for reduced selenate activity, uptake by L. pennellii LA716 was little affected by an increase in sulphate from 2.9 and 38 mM, showing that considerable variation in selectivity of the transport system for selenate versus sulphate exists among Lycopersicon species.

Salt tolerance in Aster tripolium L. III. Na and K fluxes in intact seedlings.

Uptake and transport of Na and K was studied using the radioactive tracers 22 Na and 42 K in intact Aster tripolium L. seedlings grown at two salinities CS 10 and CS 100, (containing 10mol m-1 and 100 mol m-3 Na, respectively, together with other major ions in the proportions found in sea water). At both salinities a much greater proportion of the Na than K taken up by the plant was subsequently transported to the shoot. Most 42 K fluxes were reduced by about 40% in CS 100 plants relative to CS 10 except root accumulation which increased. Experiments involving changing the salinity from CS 10 to CS 100 showed that 42 K fluxes remained constant for at least 40 h, indicating that competition with Na for uptake sites was not the cause of the reduced flux in CS 100 plants. 22 Na fluxes responded immediately to a change in salinity with all fluxes increasing six-fold when the salinity was raised. When the salinity was lowered, however, root accumulation returned to the level in CS 10 control plants whereas transport to the shoot was inhibited by the previous high salinity treatment, being reduced to only 35% of the rate in CS 10 plants. The time courses of osmotic adjustment and Na accumulation following an increase in salinity were found to be very similar, with sufficient Na being accumulated to account for the observed increase in sap osmotic pressure.

Salt tolerance in Aster tripolium L. II. Ionic regulation.

Measurements of tissue ion contents (Na, K and Cl) were carried out at frequent intervals on plants of Aster tripolium L. grown at a range of salinities for 36 d. Aster tripolium behaved as a typical halophyte showing high levels of inorganic ion accumulation even at low salinities. As salinity increased Na replaced K to a large extent in the shoot but root K was unaffected up to 500 mol m-3 external NaCl. Shoot (Na + K) concentration on a tissue water basis was maintained constant in all treatments throughout the experiment, whereas shoot (Na + K) on a dry weight basis showed marked fluctuations in some treatments. An increase in (Na + K) per gram dry weight was, however, accompanied by a parallel increase in fresh weight: dry weight (FW : DW) ratio. Transport of (Na + K) to the shoot per unit root weight changed during the experiment in the manner expected, given the observed changes in shoot relative growth rate and FW : DW to result in a constant shoot (Na + K) concentration on a water basis. Chloride was the major balancing anion in the shoot at high salinity, but never accounted for more than 38% of the (Na + K) found in the root tissue. At all salinities (Na + K) salts accounted for the majority of the measured shoot sap osmotic potential. The interactions between salinity, growth, ion transport and osmotic adjustment are discussed.

Salt tolerance in Aster tripolium L. I. The effect of salinity on growth.

A study of the growth of the maritime halophyte Aster tripolium L. has been carried out over a range of salinity treatments. The regression approach to growth analysis using frequent small harvests has been used to allow 'continuous' measurement of growth over a period of 36 d. Salinity was applied with the major ions present in ratios typical of those found in seawater. Growth was inhibited in terms of both dry weight production and leaf expansion at salinity levels equivalent to 0.625 strength sea water (full culture solution 300) and above, with the greatest effect being seen in terms of leaf area. Aster tripolium did not show increased succulence at high salinity, leaf fresh weight to dry weight ratio in fact declined, whilst leaf fresh weight per unit area remained constant. It should be noted that the plants exhibit low growth rates due to the low light intensity used.

Accessibility of phospholipids in the chromaffin granule membrane.

1. The accessibility of phospholipids in the membrane of the adrenomedullary storage vesicles (chromaffin granules) has been studied. 2. The reaction of 2,4,6-trinitrobenzenesulphonic acid with both intact granules and their ghosts, results in the labelling of 70% of the phosphatidylethanolamine. 3. The action of phospholipase A2 (from bee venom), phospholipase C (from Bacillus cereus) and sphingomyelinase C (from Staphylococcus aureus) on granules and their ghosts was followed as a function of time. No significant difference was observed between the intact granules and their ghosts. 4. In the intact granules the various treatments led to varying amounts of lysis although again no evidence was obtained that such lysis in any way increased the amount of accessible phospholipid. 5. Highly purified granule preparations were also compared with the so-called "large granule" fraction and no significant differences were detected. 6. Approx. 67% of phosphatidylethanolamine + phosphatidic acid, 50% of phosphatidylserine + phosphatidylinositol, 65% of phosphatidylcholine and 20% of sphingomyelin is accessible to enzymatic degradation. In total, approx. 50% of all the phospholipids reacted. 7. It is also shown that, unlike in enzymatic treatment, all the phosphatidylcholine can be exchanged in the presence of a phospholipid exchange protein (prepared from beef liver). 8. It is concluded that transmembrane movement of phosphatidylcholine is slow in isolated membranes of chromaffin granules. The presence of the exchange protein, however, in conjunction with membrane proteins and specific phospholipid arrangements may catalyse this transmembrane movement.