Starting from cheap inorganic salts , ultrafine P L Z T po w ders were synthesized by a co pre cipitation m ethod . The results show that the precursor precipitate obtained by the co precipita tion method transf...Starting from cheap inorganic salts , ultrafine P L Z T po w ders were synthesized by a co pre cipitation m ethod . The results show that the precursor precipitate obtained by the co precipita tion method transfor ms co m pletely to P L Z T phase by calcining at 420 ℃ for 4 hours , about300 ℃low er than the nor m al transform ation te m perature of P L Z T obtained by m ixed oxidemethod . The effect of residual N H4 N O3 in the precursor precipitate on transfor m ation te m perature of the P L Z Tpow der w as investigated . The residual N H4 N O3 in the precursor po w der can reduce further the P L Z Ttransfor m ation tem perature to about 300 ℃, but a sm alla mount of Zr O2 and Pb Ti O3 re m ained . By a proper control of the synthesizing route , a P L Z T po w der with a pri m ary particle size of 10 n m and an agglom eration size of 0 3 μm hasbeen produced .展开更多
This unique study evaluates the effects of Ralstonia solanacearum (Rs) induced biotic stress in two cultivars, Zingiber officinale (ginger) and Lycopersicon esculentum (tomato). They were grown in pots and hydroponic ...This unique study evaluates the effects of Ralstonia solanacearum (Rs) induced biotic stress in two cultivars, Zingiber officinale (ginger) and Lycopersicon esculentum (tomato). They were grown in pots and hydroponic systems with controls;to induce biotic stress, about 8 × 104 colony forming units of Rs suspension was injected into the healthy test plants. Upon induction of Rs stress, highly significant (p 0.01) biochemical changes (%) were noticed in respect to controls: carbohydrate content was generally high in both plants;while they showed decreased starch and protein contents;phenolics showed a swing of decrease or increase between pot and hydroponic systems;and all plants in general showed higher (3-6 fold) proline content upon induction of biotic stress. Regarding oxidative stress isozymes (OSE), superoxide dismutase (EC 1.15.1.1) isozymes were normally 3, but treated hydroponics had 4 with comparable relative mobility values;peroxidase (EC 1.11.1.7) isozymes were generally 2, except for treated hydroponic tomato. Briefly, Rs induced biotic stress caused wilt symptoms in ginger, but did not affect tomato though its biochemical and OSE patterns especially in those grown as hydroponics were elicited to significantly higher levels.展开更多
Na^+, Ca^+ and Mg^+ are known to be the principal mineralizing cations in oil-field waters.Chemical controls on their activity and concentration are solubility, adsorption capacity and hydration which are dependent on...Na^+, Ca^+ and Mg^+ are known to be the principal mineralizing cations in oil-field waters.Chemical controls on their activity and concentration are solubility, adsorption capacity and hydration which are dependent on the primary chemical bond parameters, such as ionic potential (Z/L)and dectronegativity (x). This paper aims at expounding the regularities governing the quantitative distribution of Na, Ca, and Mg in nil-field waters in terms of the variation of φ(Z/L, x). Our studies have shown that the log concentrations of Na, Ca and Mg in oil-field water shave a linear correlation ,vith their ionic potential and dectronegativity. Therefore, the concentrations of these cations must follow the φ(Z/L, x) regularity which has found ,vide application in the following aspects: (1) to define various types of nil-field water; (2) to define the distribution of oil-field and non-oil-field waters; and (3) to define the boundaries of hydrochemical vertical zonation.展开更多
文摘Starting from cheap inorganic salts , ultrafine P L Z T po w ders were synthesized by a co pre cipitation m ethod . The results show that the precursor precipitate obtained by the co precipita tion method transfor ms co m pletely to P L Z T phase by calcining at 420 ℃ for 4 hours , about300 ℃low er than the nor m al transform ation te m perature of P L Z T obtained by m ixed oxidemethod . The effect of residual N H4 N O3 in the precursor precipitate on transfor m ation te m perature of the P L Z Tpow der w as investigated . The residual N H4 N O3 in the precursor po w der can reduce further the P L Z Ttransfor m ation tem perature to about 300 ℃, but a sm alla mount of Zr O2 and Pb Ti O3 re m ained . By a proper control of the synthesizing route , a P L Z T po w der with a pri m ary particle size of 10 n m and an agglom eration size of 0 3 μm hasbeen produced .
文摘This unique study evaluates the effects of Ralstonia solanacearum (Rs) induced biotic stress in two cultivars, Zingiber officinale (ginger) and Lycopersicon esculentum (tomato). They were grown in pots and hydroponic systems with controls;to induce biotic stress, about 8 × 104 colony forming units of Rs suspension was injected into the healthy test plants. Upon induction of Rs stress, highly significant (p 0.01) biochemical changes (%) were noticed in respect to controls: carbohydrate content was generally high in both plants;while they showed decreased starch and protein contents;phenolics showed a swing of decrease or increase between pot and hydroponic systems;and all plants in general showed higher (3-6 fold) proline content upon induction of biotic stress. Regarding oxidative stress isozymes (OSE), superoxide dismutase (EC 1.15.1.1) isozymes were normally 3, but treated hydroponics had 4 with comparable relative mobility values;peroxidase (EC 1.11.1.7) isozymes were generally 2, except for treated hydroponic tomato. Briefly, Rs induced biotic stress caused wilt symptoms in ginger, but did not affect tomato though its biochemical and OSE patterns especially in those grown as hydroponics were elicited to significantly higher levels.
文摘Na^+, Ca^+ and Mg^+ are known to be the principal mineralizing cations in oil-field waters.Chemical controls on their activity and concentration are solubility, adsorption capacity and hydration which are dependent on the primary chemical bond parameters, such as ionic potential (Z/L)and dectronegativity (x). This paper aims at expounding the regularities governing the quantitative distribution of Na, Ca, and Mg in nil-field waters in terms of the variation of φ(Z/L, x). Our studies have shown that the log concentrations of Na, Ca and Mg in oil-field water shave a linear correlation ,vith their ionic potential and dectronegativity. Therefore, the concentrations of these cations must follow the φ(Z/L, x) regularity which has found ,vide application in the following aspects: (1) to define various types of nil-field water; (2) to define the distribution of oil-field and non-oil-field waters; and (3) to define the boundaries of hydrochemical vertical zonation.
