安全与环境学报
安全與環境學報
안전여배경학보
JOURNAL OF SAFETY AND ENVIRONMENT
2009年
6期
6-9
,共4页
蔡海洋%陈雪芸%易江婷%熊德中
蔡海洋%陳雪蕓%易江婷%熊德中
채해양%진설예%역강정%웅덕중
环境学%磷素淋失%植烟土壤%土柱%有效磷
環境學%燐素淋失%植煙土壤%土柱%有效燐
배경학%린소림실%식연토양%토주%유효린
environmentalology%phosphorus leaching%tobaccoplanting soil%soil column%available phosphorus
采用土柱淋溶模拟试验和室内培养试验,研究不同磷肥施入土壤后磷的淋失和有效磷的变化.结果表明,在施磷量为35 mg/kg条件下,整个淋洗期间,钙镁磷肥、磷酸二氢钙、磷酸一氧铵、磷酸二氢铵、磷酸二氢钾5种肥料磷的淋失率很低;各处理从上而下各层土壤的Olsen-P质量比略有增加.施磷量为60 mg/kg、110 mg/kg、170mg/kg、230 mg/kg时.潮砂田肥料磷的淋失率分别为0.26%、0.74%、2.12%和3.17%;灰泥田肥料磷的淋失率分别为0.79%、1.31%、1.60%和1.94%.钙镁磷肥施人各种土壤后,随着培养时间的延长,土壤有效磷质量比逐渐增加,80 d后达到峰值并趋于稳定;磷酸二氢钾、磷酸二氧铵、磷酸一氢铵和磷酸二氢钙施人上壤后,土壤有效磷质量比逐渐降低,至培育60 d后.变化趋于平缓.不同土壤类型对磷的吸附固定率从大到小为潮砂田、灰泥田.
採用土柱淋溶模擬試驗和室內培養試驗,研究不同燐肥施入土壤後燐的淋失和有效燐的變化.結果錶明,在施燐量為35 mg/kg條件下,整箇淋洗期間,鈣鎂燐肥、燐痠二氫鈣、燐痠一氧銨、燐痠二氫銨、燐痠二氫鉀5種肥料燐的淋失率很低;各處理從上而下各層土壤的Olsen-P質量比略有增加.施燐量為60 mg/kg、110 mg/kg、170mg/kg、230 mg/kg時.潮砂田肥料燐的淋失率分彆為0.26%、0.74%、2.12%和3.17%;灰泥田肥料燐的淋失率分彆為0.79%、1.31%、1.60%和1.94%.鈣鎂燐肥施人各種土壤後,隨著培養時間的延長,土壤有效燐質量比逐漸增加,80 d後達到峰值併趨于穩定;燐痠二氫鉀、燐痠二氧銨、燐痠一氫銨和燐痠二氫鈣施人上壤後,土壤有效燐質量比逐漸降低,至培育60 d後.變化趨于平緩.不同土壤類型對燐的吸附固定率從大到小為潮砂田、灰泥田.
채용토주림용모의시험화실내배양시험,연구불동린비시입토양후린적림실화유효린적변화.결과표명,재시린량위35 mg/kg조건하,정개림세기간,개미린비、린산이경개、린산일양안、린산이경안、린산이경갑5충비료린적림실솔흔저;각처리종상이하각층토양적Olsen-P질량비략유증가.시린량위60 mg/kg、110 mg/kg、170mg/kg、230 mg/kg시.조사전비료린적림실솔분별위0.26%、0.74%、2.12%화3.17%;회니전비료린적림실솔분별위0.79%、1.31%、1.60%화1.94%.개미린비시인각충토양후,수착배양시간적연장,토양유효린질량비축점증가,80 d후체도봉치병추우은정;린산이경갑、린산이양안、린산일경안화린산이경개시인상양후,토양유효린질량비축점강저,지배육60 d후.변화추우평완.불동토양류형대린적흡부고정솔종대도소위조사전、회니전.
This paper is entitled to study the effects of phosphorus leaching and available phosphorus in the moist sandy field or the lime marl field by means of repacked soil columns and soil-cultures. The results of our study show that, with the presence of an amount of 35 mg/kg P fertilizer, the leaching rate of phosphorus in the calcium magnesium phosphate, Ca(H_2PO_4)_2, (NH_4)_2HPO_4, NH_4H_2PO_4 and KH_2PO_4 in the moist sandy field can be reduced to a very low level whereas the Olsen-P in such treatments tends to increase slightly from the surface soil to the underground layer. In addition, the Olsen-P of different layers in various soils tend to show the following order: the lime marl field > the moist sandy field. Besides, different amounts of application also greatly affect the phosphorus leaching rates, which can be illustrated as follows: Apply phosphate fertilizer with 60 mg/kg, 110 mg/kg, 170 mg/kg, 230 mg/kg (P), and we can find that the phosphorus leaching rates in the moist sandy field and the lime marl field can be reduce to 0.26%, 0.74%, 2.12%, 3.17% and0.79%, 1.31%, 1.60%, 1.94%, respectively. The phosphorus leaching rates of the moist sandy field tend to be lower than that in the lime marl field when 0 mg/kg, 60 mg/kg, 110 mg/kg (P) applied. In case the calcium magnesium phosphate is applied to all the above soils, with the time extension, the content of soil's available phosphate would increase gradually whereas the soil tends to be stable in 80 days if it received the highest amount of available phosphate. The content of the soil's phosphate available would gradually decrease when Ca (H_2PO_4 )_2, ( NH_4 )_2HPO_4, NH_4H_2PO_4 and KH_2PO_4 were applied to the above soils. Thus, it can be seen that the change of the P content proves to be minor and therefore tended to be stabilized. The P fixation ratios of different phosphorus fertilizers in various soils were found to obey the following order: the moist sandy field > the lime marl field.