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Characterization and greenhouse evaluation of Brazilian calcined nonapatite phosphate rocks for rice

机译:巴西煅烧非磷灰石磷酸盐岩水稻的特征特性及温室效应评价

摘要

Little information is available on the agronomic effectiveness of calcined nonapatite phosphate rock (PR) sources containing crandallite minerals in the form of Ca-Fe-Al-P for flooded and upland rice (Oryza sativa L.). We conducted laboratory and greenhouse studies to (i) characterize the mineralogical composition, (ii) investigate the solubility and dissolution behavior, and (iii) evaluate the agronomic effectiveness of two nonapatite PR sources (Juquia and Sapucaia) from Brazil and compared them with (i) a highly reactive Gafsa PR (Tunisia) containing apatite in the form of Ca-P and (ii) a reference water-soluble triple superphosphate (TSP) for flooded and upland rice. After calcination at 500 degrees C for 4 h, the solubility of Juquia PR and Sapucaia PR in neutral ammonium citrate (NAC) significantly increased from almost nil to a maximum of 39.3 and 114 g P kg(-1), respectively. X-ray diffraction showed that crystalline crandallite mineral was transformed to an amophorus form after calcination. The solubility behavior of the two calcined PR sources followed the same trend as Gafsa PR, that is, P release decreased with increasing equilibrium pH in the 0.01 M KCl solution (PH 3.0-8.0). At PH 3, the solubility followed: Gafsa PR > calcined Sapucaia PR > calcined Juquia PR. No P release was detected from any of the PR sources at pH >= 5.0 in the solution, indicating the Ca-P characteristic of the Ca-Fe-Al-P mineral controlled P dissolution of the calcined PR. Without calcination, both Juquia PR and Sapucaia PR were totally ineffective for upland rice grown on a Hiwassee clay loam (fine, kaolinitic, thermic Rhodic Kanhapludult) with pH 5.4 whereas a significant P response was observed with the calcined PR samples. For flooded rice grown on Hiwassee soil, the calcined Juquia PR and Sapucaia PR were 66 and 72%, respectively, as effective as TSP in increasing rice grain yield whereas Gafsa PR was ineffective. For upland rice grown on the unlimed soil, Gafsa PR was as effective as TSP in increasing rice grain yield whereas calcined Juquia PR and Sapucaia PR were 89 and 83% of TSP. The effectiveness of Gafsa PR was reduced to 0% after the soil was limed to pH 7.0 whereas the two calcined PR sources were reduced to 49% of TSP. Soil available P extracted by iron oxide impregnated filter paper (Pi test) or anion-exchange resin after rice harvest correlated well with P uptake by rice grain for flooded and upland rice.
机译:关于煅烧的非磷灰石磷酸盐岩(PR)来源,以Ca-Fe-Al-P形式存在的方铁石矿物,对淹水和旱稻(Oryza sativa L.)的农艺有效性几乎没有信息。我们进行了实验室和温室研究,以(i)表征矿物成分,(ii)研究溶解度和溶解行为,(iii)评估来自巴西的两种非磷灰石PR来源(Juquia和Sapucaia)的农艺学有效性,并将其与( i)具有Ca-P形式磷灰石的高反应性Gafsa PR(突尼斯),以及(ii)用于淹水和旱稻的参考水溶性三重过磷酸钙(TSP)。在500摄氏度下煅烧4小时后,Juquia PR和Sapucaia PR在中性柠檬酸铵(NAC)中的溶解度从几乎为零显着增加至最大39.3和114 g P kg(-1)。 X射线衍射表明,煅烧后结晶的方钠石矿物质转化为氨水形式。两种煅烧PR源的溶解度行为遵循与Gafsa PR相同的趋势,即,随着0.01 M KCl溶液(PH 3.0-8.0)中平衡pH的增加,P的释放减少。在PH 3时,溶解度如下:Gafsa PR>煅烧的Sapucaia PR>煅烧的Juquia PR。在溶液中pH> = 5.0时,未从任何PR源中检测到P释放,表明煅烧PR的Ca-Fe-Al-P矿物控制P溶解的Ca-P特性。如果不进行煅烧,Juquia PR和Sapucaia PR都对在pH值为5.4的Hiwassee粘土壤土(细,高岭土,热的Rhodic Kanhapludult)上生长的旱稻完全无效,而煅烧的PR样品观察到显着的P响应。对于生长在希瓦瑟湖土壤上的淹水水稻,煅烧后的Juquia PR和Sapucaia PR分别与TSP一样有效提高稻谷产量,而Gafsa PR无效。对于在无盐土壤上生长的旱稻,Gafsa PR在提高稻谷产量方面与TSP一样有效,而煅烧的Juquia PR和Sapucaia PR则占TSP的89%和83%。将土壤灰化至pH 7.0后,Gafsa PR的有效性降低到0%,而两种煅烧的PR来源降低到TSP的49%。水稻收获后,用氧化铁浸渍滤纸(Pi试验)或阴离子交换树脂提取的土壤有效磷与水稻籽粒对水淹和旱稻的磷吸收有很好的相关性。

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