Availability of Ca from Ca45SO4 in a highly saline-sodic soil

Summary Application of gypsum (tagged Ca⁴⁵SO₄.2H₂O) caused a considerable increase in dry matter yield and content of Ca, Ca⁴⁵, Mg and K and Ca:Na and (Ca+Mg): (Na+K) ratios and a decrease in the content of Na, N and P in dhaincha tops. There was a considerable increase in the total uptake of Ca, Mg, Na, K, N, P and Ca⁴⁵ by plant tops in response to gypsum. Contribution of Ca from applied Ca⁴⁵SO₄ varied from 78.3 to 84.7 per cent of the total Ca in plant tops, whereas, its uptake from this source varied from 52.18 to 98.73 me per 100 g plant tops. re]19720705     

Relationships between plasma composition and parotid salivary composition and secretion rates in the potoroine marsupials,Aepyprymnus rufescens and Potorous tridactylus

Summary Parotid salivation was investigated in two species of potoroine marsupial, Aepyprymnus rufescens and Potorous tridactylus to ascertain flow rates and composition, the buffer capacity of the saliva with respect to possible dependence of these animals on foregut fermentation, and the similarity of anion excretion patterns to those of the kangaroo parotid. Under anaesthesia neither species secreted spontaneously and secretion was stimulated by intravenous infusion of carbachol, bethanechol and isoprenaline. Under cholinergic stimulation in Aepyprymnus, the concentrations of Na, Cl, HCO₃ and osmolality were positively correlated with flow rate, whereas K, Mg, PO₄, H⁺ and urea were negatively correlated with flow. Amylase activity and the concentrations of protein and Ca showed no consistent relation to flow. Relative to Aepyprymnus, saliva of Potorous had much lower amylase activity and amylase activity per gram protein, lower concentrations of urea and Ca, and higher Na. Protein, K and HCO₃ concentrations were similar in both species. The plasma of both species had similar electrolyte concentrations, but Potorous had lower protein, urea, osmolality and amylase activity. Plasma amylase activity in Aepyprymnus rose during cholinergic stimulation to levels in excess of rodent plasma. Isoprenaline infusion in Aepyprymnus increased salivary amylase activity and concentrations of protein, Ca, HCO₃ and PO₄, and reduced the concentrations of Cl and H⁺. The patterns of anion excretion in the two potoroine marsupials were dissimilar to those of the kangaroo parotid suggesting that parotid fluid secretion is not HCO₃ driven to the same extent as that of kangaroos. Buffer anion concentrations and secretion rates were similar to koalas and low relative to kangaroos, indicating that these potoroines do not rely on foregut fermentation.Abbreviations bw body weight - SEM standard error of mean - VFA volatile fatty acids     

Osmotic diuresis and its effect on total electrolyte distribution in plasma and urine of the aglomerular teleost,Lophius americanus

Quantitative evaluations have been made of the chief anions and cations in plasma, urine, and pericardial fluid taken both from freshly captured goosefish and from those undergoing "laboratory diuresis." Measurements included: Na, K, Ca, Mg, Cl, SO₄, PO₄, protein, HCO₃, NH₃, pH, titratable acidity, freezing point depression, creatine, trimethylamine oxide, and plasma volume. The total patterns of electrolyte distribution in these body fluids are presented. The morphologically undifferentiated aglomerular tubule acts as a barrier to the free diffusion of monovalent electrolytes, while transporting actively the divalent ions, especially Mg. Urine taken from freshly captured fish is hypotonic to plasma, low in electrolyte, and as much as 50 per cent of its total osmolarity is accounted for by nitrogenous components. Of these creatine is transported most actively by the renal tubule cells. With the onset of diuresis immediately after capture, plasma osmolarity slowly rises and urine suddenly becomes isotonic with plasma as chloride floods into the urine. The active movement of Mg continues during diuresis and urine/plasma concentration ratios of 100 or more are sustained for days while the animals are kept in the laboratory. Na follows chloride and never reaches 50 per cent of plasma values, and K never appears in urine in more than mere traces. Electrolytes in this system are viewed as not being in true equilibrium but rather as constituting a biological steady state with the distribution across renal cells being maintained against passive diffusion by the expenditure of cellular energy.     

Identification of major sources controlling groundwater chemistry from a multilayered aquifer system

Abstract

The Maknassy basin is a typical example of an arid area in Central Tunisia. The geology of the area is mainly composed of Cretaceous calcareous formations. To identify the major process involved in controlling the groundwater chemistry, 53 groundwater samples for three different aquifer levels have been examined. The groundwater chemistry is dominated by SO₄ (Na + Mg) and (Cl + SO₄). The presence of (Ca + Mg) and (Na + K) with HCO₃ indicates the domination of dolomitic rock weathering as the major source of cations. The plots for Na to Cl indicate a fine correlation and reflects their release from halite dissolution during groundwater transition. An ion exchange process is also activated in study area which is indicated by a shift to the right in a plot for Ca + Mg to SO₄ + HCO₃. The plot of Na – Cl to Ca + Mg – (HCO₃ + SO₄) confirms that Ca, Mg and Na concentrations in groundwater are derived from aquifer materials. Saturation indexes of groundwater samples indicate undersaturation for gypsum and anhydrite, and oversaturation for calcite, dolomite and aragonite confirming waterrock interactions by dissolution and dilution processes. In general, water chemistry is guided by weathering process, ion exchange and water-rock interaction during groundwater transition.     

The chemistry of surface water in prairie ponds

Water analyses from 80 small prairie ponds, 0.17 to 89.8 hectares, in Manitoba and Saskatchewan between 1967 to 1972 exhibited two basic ionic dominance patterns HCO₃ > SO₄ > Cl and SO₄ > HCO₃ > Cl. The order of SO₄ and Cl were reversed in 40 percent of the bicarbonate ponds below 500 µmhos/cm. At salinities above 12,000 µmhos/cm, Cl exceeds SO₄ in several wetlands. Temporary wetlands were characterised by Ca > K > Mg > Na / HCO₃ > Cl > SO₄, semi-permanent ponds Mg > Ca > Na > K / SO₄ > HCO₃ > Cl while the permanent pond structure was Ca > Mg > Na > K / HCO₃ > SO₄ > Cl.Conductivities of the wetlands studied ranged from 47 to 23,000 µmhos / cm.Seasonal changes in salinity varied within and between pond types as well as from year to year. The average salinity increase within season in temporary ponds was 67 percent, 63 percent in semi-permanent ponds and 20 percent for permanent ponds. These changes were affected by evaporation, transpiration, see-page and precipitation patterns. Ionic dominance patterns did not change within a season although Mg, K and HCO₃ increased at higher rates than Ca, Na, CI and SO₄.Temporary wetlands are slightly acidic, averaging pH 6.8 while semi-permanent and permanent ponds were alkaline, pH range 7.1 to 9.2. No stratification of pH with depth and minimal diurnal variation was recorded.At two study areas, Bradwell and St. Denis fhe following ranges (micrograms/litre) were recorded: 3 to 630 PO₄-P, 10 to 650 NO₃-N, 5 to 630 TDFe, 1 to 13 TDCu and 1 to 27 TDZn. Colour was 5 to 190 Hazen units at St. Denis and 10 to 110 for Bradwell.Two herbicides, 2,4-D and 2,4,5-T were detected at levels of 4 to 111 and 1.4 to 13.5 micrograms/litre, respectively, from 15 ponds at St. Denis.     

THE PENETRATION OF AMMONIA INTO FROG MUSCLE

1. A study was made of the electrolyte changes which occur when frog muscles are immersed in a Ringer solution with 1/5 of the Na replaced by NH₄Cl. Analyses were made in the solution and in the muscles for K and NH₃, and the muscles were also analyzed for Cl, HCO₃, and Na. Control muscles were immersed in normal Ringer''s solution and similarly analyzed. 2. The amount of ammonia taken up was about equal to the K and Na lost. There was also a small increase in chloride content. The bicarbonate content was the same in both experimental and control muscles, indicating no change in the muscle pH due to the NH₃ which penetrated. An increased loss of K due to the penetration of NH₃ was also demonstrated by the use of radioactive K. 3. After 5 hours, the concentration of ammonia per gram of muscle is about the same as the concentration in the solution. After 4 or 5 days, the concentration in the muscle is about 1.5 times that in the solution. The inside to outside NH₃ ratio is about equal to the corresponding H ion ratio, but is much less than the K ratio. 4. The rate of penetration of the NH₃ is increased by a rise of temperature, by stirring the solution, and by decrease in the concentration of Na, K, Ca, or Mg in the solution; it is decreased by increasing the size of the muscles or by killing them with chloroform or boiling. 5. Liver, smooth muscle, skin, and kidney, in a few experiments, behaved much like muscle except that there was a formation of urea in the case of liver. 6. The injection of NH₄Cl into anesthetized cats causes an increase in the level of K in the blood plasma.     

Renal Calculi

The pathogenesis of renal calculi is reviewed in general terms followed by the results of investigation of 439 patients with renal calculi studied by the author at Toronto General Hospital over a 13-year period. Abnormalities of probable pathogenetic significance were encountered in 76% of patients. Idiopathic hypercalciuria was encountered in 42% of patients, primary hyperparathyroidism in 11%, urinary infection in 8% and miscellaneous disorders in 8%. The incidence of uric acid stones and cystinuria was 5% and 2% respectively. In the remaining 24% of patients in whom no definite abnormalities were encountered the mean urinary magnesium excretion was less than normal. Of 180 patients with idiopathic hypercalciuria, only 24 were females. In the diagnosis of hyperparathyroidism, the importance of detecting minimal degrees of hypercalcemia is stressed; attention is also drawn to the new observation that the upper limit of normal for serum calcium is slightly lower in females than in males. The efficacy of various measures advocated for the prevention of renal calculi is also reviewed. In the author''s experience the administration of thiazides has been particularly effective in the prevention of calcium stones. Thiazides cause a sustained reduction in urinary calcium excretion and increase in urinary magnesium excretion. These agents also appear to affect the skeleton by diminishing bone resorption and slowing down bone turnover.     

Changes in nuclear electrolytes of Chironomus thummi salivary gland cells during development

A technique is described for the measurement of Na⁺, K⁺ and Mg²⁺ in cytoplasmic samples and nuclei from chironomid salivary glands. [Na], [K] and [Mg] were followed from the penultimate (L₃) through the last larval instar (L₄) until pupation, in the two developmental types, R and B, of Chironomus thummi. In nuclei, [Mg] falls from 78 mM in the middle of the L₃ to about 27 mM at the L₃ → L₄ molt, a level which is maintained thereafter. [Na] falls from 180 mM to around 60 mM at the L₃ → L₄ molt and falls further to about 38 mM in the prepupa; the pattern of change differs between the developmental types. [K] increases at both molts, from a level of 131 mM to about 150 mM at the L₃ → L₄ molt and from about 115 mM to about 130 mM at the pupal molt, the developmental types differing again. The cytoplasmic ion content measured during the prepupal stage runs parallel to the nuclear samples but always contains about 18 mM more Na and 12 mM less K than the nuclei. In the nuclei the ∑[Na + K] has a steady downward trend but rises slightly in the prepupa. The Na/K ratio follows a complex course related to the molt cycles. Analysis of variation allows to discern subclasses of nuclei with a particularly high Na/K ratio; the frequency of such nuclei is followed through development. It is argued (a) that the observed alterations in cation composition are of a kind and magnitude which under experimental conditions can induce puffs in certain chromosomal segments, and (b) that shifts in ion concentration may be implicated in the control of DNA replication.     

Increasing phosphorus concentration in the extraradical hyphae of <Emphasis Type="Italic">Rhizophagus irregularis</Emphasis> DAOM 197198 leads to a concomitant increase in metal minerals

Plants associated with arbuscular mycorrhizal fungi (AMF) acquire phosphorus via roots and extraradical hyphae. How soil P level affects P accumulation within hyphae and how P in hyphae influences the accumulation of metal minerals remains little explored. A bi-compartmented in vitro cultivation system separating a root compartment (RC), containing a Ri T-DNA transformed carrot root associated to the AMF Rhizophagus irregularis DAOM 197198, from a hyphal compartment (HC), containing only the extraradical hyphae, was used. The HC contained a liquid growth medium (i.e., the modified Strullu-Romand medium containing P in the form of KH₂PO₄) without (0 μM) or adjusted to 35, 100, and 700 μM of KH₂PO₄. The accumulation of P and metal minerals (Ca, Mg, K, Na, Fe, Cu, Mn) within extraradical hyphae and AMF-colonized roots, and the expression of the phosphate transporter gene GintPT were assessed. The expression of GintPT in the extraradical hyphae did not differ in absence of KH₂PO₄ or in presence of 35 and 100 μM KH₂PO₄ in the HC but was markedly reduced in presence of 700 μM KH₂PO₄. Hyphal P concentration was significantly lowest in absence of KH₂PO₄, intermediate at 35 and 100 μM KH₂PO₄ and significantly highest in presence of 700 μM KH₂PO₄ in the HC. The concentrations of K, Mg, and Na were positively associated with the concentration of P in the extraradical hyphae developing in the HC. Similarly, P concentration in extraradical hyphae in the HC was related to P concentration in the growth medium and influenced the concentration of K, Mg, and Na. The accumulation of the metal mineral K, Mg, and Na in the extraradical hyphae developing in the HC was possibly related to their function in neutralizing the negative charges of PolyP accumulated in the hyphae.     

Municipal wastewater treatment with vertical flow constructed wetlands for irrigation reuse

The treatment effect of two pilot-scale vertical flow constructed wetlands (VFCWs) on municipal wastewaters and their suitability for irrigation reuse were evaluated in a 2-year (2002–2003) experiment. One VFCW was planted with Typha latifolia and the other with Phragmites australis. VFCW efficiency was evaluated in terms of both mass removal and water quality improvement, considering the following parameters: pH, electrical conductivity (EC_w), total suspended solids (TSS), chemical oxygen demand (COD) and biochemical oxygen demand (BOD), total nitrogen (TN) and nitrate (NO₃^?), total phosphorus (TP) and orthophosphate (PO₄^3?), sodium (Na), potassium (K), magnesium (Mg) and calcium (Ca). The accumulation of the elements in the plant organs and VFCW sandy surface layer and their offtake with the macrophyte harvest were also measured.In quantitative terms the established VFCWs showed higher removal efficiencies (>86%) for COD, BOD, N and K, while lower efficiencies (<47%) were observed for Na and Mg. The direct contribution (offtake) of the macrophytes in N, P and K removal processes was particularly high (>65%) due to the massive growth. The results were less favourable in terms of water quality, because the high evapotranspiration losses counteracted the depuration process by concentrating the elements in the outflow water. Higher concentrations were found in outflow than inflow, especially of Na (relative increase of 89%) and Mg (relative increase of 74%). Only parameters with high removal efficiencies fulfilled the Italian guidelines for irrigation reuse whereas parameters with lower efficiencies (e.g., TSS, TP) limited the potential water reuse. Efficient pre-cleaning systems or innovative integrated systems are thus necessary to obtain high removal efficiencies that reduce the effect of ET on water quality.     

Characterization of wheat germ lipase

Some properties of wheat germ lipase were determined with a fluorometric assay of enzymatic cleavage converting the nonfluorescent 4-methyl umbelliferone butyrate (4-MUB) to the highly fluorescent 4-methyl umbelliferone (4-MU). Optimum reaction conditions were attained at buffer pH 7·5 and temperature 30°. Lineweaver-Burk plots were linear. Relative cation combination effectiveness as reaction activators was Ca + Mg + K > Ca + Mg + K + Na > Ca + Mg + Na > Ca + Mg > Mg > Ca, with no reaction effects of K, Na, and K + Na without Ca or Mg. Highly significant inhibitors of lipase reaction were CN⁻, aflatoxin, Cu²⁺, Fe³⁺, S²⁻, and EDTA.     

Angiotensin-converting enzyme and metals in untreated essential hypertension

Hpertension is an important health problem throughout the world and a risk factor for many diseases. Angiotensin-converting enzyme (ACE), a component of the renin-angiotensin system, has an important role in the regulation of blood pressure. Zinc (Zn), a trace element with important biological functions, is located in the catalytic site of ACE. Calcium (Ca), magnesium (Mg), sodium (Na), and potassium (K) also appear to be involved in hypertension pathogenesis. In this study, plasma ACE activities and Ca_t, Ca_i, Mg, Na, K, and plasma/erythrocyte Zn levels of 20 untreated patients with essential hypertension and 28 helthy individuals were evaluated. Plasma ACE activities (p<0.05) and erythrocyte Zn concentrations (p<0.001) were significantly higher in patients with essential hypertension than values of the control group. No significant difference was found between plasma Zn concentrations of the groups (p>0.05). Plasma Ca_t (p<0.001) and Mg levels (p<0.05) in essential hypertension were significantly lower than those of controls. Plasma Na, K, and Ca_i levels remained normal in essential hypertension. There are complex associations between metals and arterial pressure. Ca and Mg deficiencies seem to be associated with increased prevalence of hypertension. Increases in erythrocyte Zn may have a future potential use for diagnosis of hypertension.     

Potassium and other minor elements in Porites corals: implications for skeletal geochemistry and paleoenvironmental reconstruction

We investigated how the K/Ca, Na/Ca, Mg/Ca, and Sr/Ca ratios of powders ground from Porites coral skeletons are changed by cumulative chemical treatments to the powders: first with distilled/deionized water (DDW), next with 30?% H₂O₂ and then with 0.004?mol?l^?1 HNO₃. The K/Ca, Na/Ca, and Mg/Ca ratios were decreased with the DDW treatment and then increased with the H₂O₂ and HNO₃ treatments; the Sr/Ca ratio was slightly decreased through the cumulative treatments, suggesting fine-scale (tens of ??m or less) elemental heterogeneities in the skeleton??K, Na, and Mg are significantly enriched at the skeletal surface and also at the center of calcification (COC); in contrast, the heterogeneity of Sr is very small. We suggest that the principal mechanisms of K incorporation into coral skeleton are (1) ion incorporation into lattice defects/distortions and (2) ion adsorption onto crystal discontinuities (including crystal?Corganic matter interfaces) as forms of K⁺ and KSO₄ ^?. Furthermore, we measured the element/Ca ratios of a modern Porites coral skeleton along its growth direction at 2-mm intervals. Results showed that all the element/Ca ratios displayed annual cycles, that the K/Ca and Na/Ca ratios covaried with each other, and that the annual-minimum K/Ca and Na/Ca ratios coincided with the annual high-density band in the skeleton. It is unclear what environmental factors may cause the covarying annual cycles of the K/Ca and Na/Ca ratios; however, as a possible explanation, the cycles may be due not to environmental factors, but to a combined effect of (1) the K and Na enrichment at the COC, (2) annual bands of high- and low-density skeleton, and (3) mm-scale element/Ca measurements along the skeletal growth direction. This kind of effect on geochemical proxies of which the concentrations significantly differ between the COC and surrounding skeleton may generate false or distorted paleoenvironmental signals.     

Influence of the explantation milieu on intranuclear (Na), (K) and (Mg) of Chironomus thummi salivary gland cells

Intranuclear Na, K and Mg concentrations were determined in cells of salivary glands incubated for 1^h in selected NaCl/KCl/MgCl₂ media. By variation of the external milieu beyond “physiological” limits the intranuclear electrolytes can be shifted between ca 100 and 280 mM [K]ⁱ, between ca 8 and 100 mM [Na]ⁱ and between ca 5 and 75 mM [Mg]ⁱ. No significant competition or interactions of the 3 ionic species are apparent. The relationships [K]^e : [K]ⁱ and [Na]^e : [Na]ⁱ can best be described by a positive and linear, that between [Mg]^e : [Mg]ⁱ by a negative and exponential function. Regression parameters are given which permit a computation of intranuclear [Na], [K] and [Mg] as induced by NaCl/KCl/MgCl₂ in any binary or triple combination that is tolerated by the explanted gland without visible damage.     

Different types of hypercalciuria in patients with renal lithiasis and evidence of the calcium renal waste

A study of normal subjects and patients with hypercalciuria and recurrent renal stones has identified three main types of hypercalciuria: complex, absorptive and renal. Complex hypercalciuria is a combination of absorption, renal leak and resorption factors. Absorption and renal leak were examined by means of a 45Ca test. Resorption is defined as an increase of the urinary calcium:creatinine ratio while the subjects are being maintained on an intake of 400 mg of calcium per 24 h.     

Changes in osmolality and blood serum ion concentrations in pregnancy

Changes in osmolality and the concentration of cations (Na, K, Ca, Mg) were studied in blood serum of pregnant women from two weeks after conception, throughout the whole pregnancy, and within the first week after delivery. Altogether 239 women from 18 to 40 years of age were studied. Blood serum osmolality decreased from 287±0.8 to 278±1.6 mOsm/kg H₂O from the fifth week of pregnancy and remained virtually at this level until the end of pregnancy. Hyponatremia was found during the three trimesters of pregnancy, in trimesters II and III hypokalemia was not observed, whereas hypocalcemia and hypomagnemia were found. On the first day after delivery, the blood serum osmolality and concentrations of magnesium ions returned to their levels in nonpregnant women, whereas concentrations of sodium and calcium ions remained decreased. No correlation was found between hypoosmia and changes in blood serum concentrations of ions under study during the three trimesters of pregnancy. Thus, in normal pregnancy, hypoosmia develops from the fifth week after conception and persists until delivery. The concentrations of sodium, potassium, calcium, and magnesium ions are regulated by independent mechanisms to provide retention of these parameters within certain periods of pregnancy at the level of nonpregnant women on the background of hypoosmia.     

Accession and cycling of elements in a coastal stand ofPinus radiata D. Don in New Zealand

Summary The accession and cycling of elements in a 14-year-old coastal stand ofPinus radiata D. Don was measured for one year. The element contents (mg m^–2 year^–1) of bulk precipitation and throughfall respectively were: NO₃–N 41, 12; NH₄–N 133, 154; organic-N 157, 396; Na 4420, 9700; K 387, 2900; Ca 351, 701; Mg 486, 1320. Of the increase in element content of rainwater beneath the forest canopy 20% (NH₄–N), 70% (organic-N), 3% (Na), 90% (K), 20% (Ca) and 30% (Mg) was attributed to leaching; the remainder to washing of aerosols filtered from the atmosphere by the vegetation. The canopy absorbed approximately 40 mg m^–2 year^–1 of NO₃–N. Litterfall was the major pathway for the above-ground biogeochemical cycle of N (93%), Ca (96%) and Mg (74%), and leaching was the major (73%) pathway for K.     

Urease activity in soils

Summary The availability of Ca from different levels of gypsum and calcium carbonate in a non-saline sodic soil has been investigated. Different levels of tagged gypsum (Ca⁴⁵SO₄.2H₂O) and calcium carbonate (Ca⁴⁵CO₃) (i.e. 0, 25, 50, 75, and 100 per cent of gypsum requirement) were mixed thoroughly in 3.5 Kg of a non-saline alkali soil (ESP, 48.4; ECe, 2.68 millimhos/cm). Dhaincha (Sesbania aculeata) — a legume and barley (Hordeum vulgare L.) — a cereal were taken as test crops. Increasing levels of gypsum caused a gradual increase in the yield of dry matter, content of Ca and K in the plant tops and Ca:Na and (Ca+Mg):(Na+K) ratios in both the crops. Application of calcium carbonate caused a slight increase in the dry matter yield, content of Ca and Mg and Ca:Na and (Ca+Mg):(Na+K) ratios in barley, however, in case of dhaincha there was no such effect. Gypsum application caused a gradual decrease in the content of Na and P in both the crops. Total uptake of Ca, Mg, K, N and P per pot increased in response to gypsum application. The effect of calcium carbonate application on the total uptake of these elements was much smaller on dhaincha, but in barley there was some increasing trend.Increasing application of tagged gypsum and calcium carbonate caused a gradual increase in the concentration and per cent contribution of source Ca in both the crops, although, the rate of increase was considerably more in dhaincha. The availability of Ca from applied gypsum was considerably more than that from applied calcium carbonate. Efficiency of dhaincha to utilize Ca from applied sources was considerably more (i.e. about five times) than that of barley     

Studies on the heat-precipitated phosphoenzyme complex of eel electric organ (Na + K).ATPase.

When the hydrolytic reaction between eel electric organ (Na + K) · ATPase and [γ-³²P]ATP is terminated at neutral pH by heat precipitation, a phosphoenzyme complex is formed which reaches maximal levels in the simultaneous presence of Mg, Na, and K. After formation of a steady-state level of phosphoenzyme in the presence of Mg and Na, a pulse of K increases the level of the heat-precipitated phosphoenzyme (while decreasing the level of the acid-precipitated phosphoenzyme). The formation of the heat-precipitated phosphoenzyme is clearly inhibited by ouabain only when the phosphoenzyme is formed in the presence of Mg, Na, and K. Inorganic phosphate decreases the level of the heat-precipitated phosphoenzyme, but not that of the acid-precipitated phosphoenzyme (in the presence of Mg and Na or in the presence of Mg, Na, and K). Moreover, a heat-precipitated, ouabain-sensitive phosphoenzyme forms in the reaction between the eel (Na + K) · ATPase and ³²P_i with or without ATP. The pH stability of the heat-precipitated phosphoenzyme complex is maximal at pH 6 to 8, and this complex shows little or no reactivity with neutral hydroxylamine, suggesting that the phosphate is not bound to an acyl residue of the protein. These experiments indicate that both heat-resistant and acid-resistant phosphoenzymes are formed during the (Na + K) · ATPase reaction at pH 7.4.     

Effect of N,K, and P fertilization,N source,and clipping on potential tetany hazard of bromegrass

Summary The objective of this field study was to determine early-season effects of N source, N, K, and P fertilization, and clipping (to simulate grazing) on potential tetany hazard of bromegrass (Bromus inermis L.) as indicated by the chemical composition of its forage. Tetany is a metabolic disorder of ruminants resulting from forage with low Mg availability. Chemical components considered in the forage were inorganic cations, organic acids, aconitate, and per cent total N/per cent total water soluble carbohydrate (N/TWSC). Differences between the sum (in meq/kg) of inorganic cations (Mg, Ca, K, and Na) and inorganic anions (Cl, NO₃, H₂PO₄, and SO₄) in forage were defined as the concentration of organic acids (C-A). Soil was Parshall fsl, a Pachic Haploboroll. Yields and chemical composition of oven-dried forage from previously unclipped and reclipped plots were determined at 3-week intervals beginning May 22 and June 12, respectively. A water budget was determined using soil-water and rainfall data.Forage yields were increased 2- to 3-fold by N fertilization with the NO₃-N source generally outyielding the NH₄-N source. A slight additional yield response to that obtained with N alone was obtained with K+P fertilization but not with K or P alone with or without N. Much less total forage was removed from reclipped plots than from unclipped plots. Forage Mg content was decreased only slightly by K or NH₄-N fertilization. Soil analysis indicated that high NH₄-N levels were present at the May 22 harvest. Magnesium and Ca concentrations were only slightly affected by N fertilization; however, K, K/(Ca+Mg), total N, C-A, and aconitate were increased. Reclipping increased Mg, N, K, N/TWSC, C-A, and aconitate. Estimates of blood-plasma Mg concentrations were obtained by using the data for plant N, K, and Mg. These estimates did not indicate increased tetany hazard as a result of reclipping, but did indicate increased tetany hazard from N fertilization. Forage C-A and aconitate concentrations were decreased by fertilization with KCl which seemed to have been caused by the increased Cl concentrations in the forage. Estimates of quantities of Mg, arriving at the root surfaces from the soil by mass flow, far exceeded amounts of Mg in the forage. Mass flow seemed to be the principal mechanism by which Mg and Ca arrived at root surfaces but this mechanism was much less important for K.This study indicated an increased potential tetany hazard resulting primarily from N fertilization with either NH₄-N or NO₃-N sources. However, the potential for increased forage and livestock-carrying capacity with N fertilization is very large. Therefore, management practices corroborated by livestock data are vitally needed to minimize tetany hazard while increasing bromegrass yields by N fertilization.Contribution from Soil, Water, and Air Sciences, North Central and Northeastern Regions, ARS-USDA.Follett, Power, and Grunes are soil scientists and Kleinis a biological laboratory technician. Follett is now National Program Staff Scientist, ARS, BARC-West, Beltsville, MD 20705. Power and Klein are at the USDA Northern Great Plains Research Center, Mandan, ND 58554, as formerly was Follett. Grunes is at the U.S. Plant, Soil and Nutrition Laboratory, Ithaca, NY 14853.