西南师范大学学报(自然科学版)
西南師範大學學報(自然科學版)
서남사범대학학보(자연과학판)
JOURNAL OF SOUTHWEST CHINA NORMAL UNIVERSITY
2015年
1期
58-64
,共7页
肖懿%唐家良%朱波%王芮%王艳强
肖懿%唐傢良%硃波%王芮%王豔彊
초의%당가량%주파%왕예%왕염강
紫色土%磷素吸附解吸%土地利用类型
紫色土%燐素吸附解吸%土地利用類型
자색토%린소흡부해흡%토지이용류형
purple soil%phosphorus adsorption-desorption%land use
磷素是水体富营养化的重要限制营养元素,农地磷肥过量施入造成的磷流失导致水污染问题引起世界范围的普遍关注。本研究主要针对紫色土集中分布的四川盆地丘陵区土地利用方式多样、农业非点源污染显著等特点,采集不同土地利用方式(林地、坡耕地)下的典型酸性、中性及石灰性紫色土,开展磷素等温吸附解吸热力学实验,并结合L ang m uir模型研究了不同类型紫色土对磷素的吸附-解吸特征的影响。结果表明,四川盆地丘陵区紫色土林地土壤磷素最大吸附量(Qm)及磷吸附缓冲容量(MBC)高于同类型紫色土农地土壤;林地土壤生物有效磷含量低于农地;农地磷素释放风险高于林地。相较中性及石灰性紫色土,酸性紫色土磷素最大吸附量、吸附缓冲容量低,但磷素解吸能力较高,表明酸性紫色土磷素释放风险较大。多重相关分析表明,尽管不同类型紫色土pH、有机质、土壤质地等因素对磷素吸附解吸并无单一的显著影响,从而无法针对所有3种土壤找出其影响磷素吸附解吸的共性因素,但因子分析结果表明pH、土壤质地及土壤总磷含量对磷素吸附解吸特性仍有直接影响。
燐素是水體富營養化的重要限製營養元素,農地燐肥過量施入造成的燐流失導緻水汙染問題引起世界範圍的普遍關註。本研究主要針對紫色土集中分佈的四川盆地丘陵區土地利用方式多樣、農業非點源汙染顯著等特點,採集不同土地利用方式(林地、坡耕地)下的典型痠性、中性及石灰性紫色土,開展燐素等溫吸附解吸熱力學實驗,併結閤L ang m uir模型研究瞭不同類型紫色土對燐素的吸附-解吸特徵的影響。結果錶明,四川盆地丘陵區紫色土林地土壤燐素最大吸附量(Qm)及燐吸附緩遲容量(MBC)高于同類型紫色土農地土壤;林地土壤生物有效燐含量低于農地;農地燐素釋放風險高于林地。相較中性及石灰性紫色土,痠性紫色土燐素最大吸附量、吸附緩遲容量低,但燐素解吸能力較高,錶明痠性紫色土燐素釋放風險較大。多重相關分析錶明,儘管不同類型紫色土pH、有機質、土壤質地等因素對燐素吸附解吸併無單一的顯著影響,從而無法針對所有3種土壤找齣其影響燐素吸附解吸的共性因素,但因子分析結果錶明pH、土壤質地及土壤總燐含量對燐素吸附解吸特性仍有直接影響。
린소시수체부영양화적중요한제영양원소,농지린비과량시입조성적린류실도치수오염문제인기세계범위적보편관주。본연구주요침대자색토집중분포적사천분지구릉구토지이용방식다양、농업비점원오염현저등특점,채집불동토지이용방식(임지、파경지)하적전형산성、중성급석회성자색토,개전린소등온흡부해흡열역학실험,병결합L ang m uir모형연구료불동류형자색토대린소적흡부-해흡특정적영향。결과표명,사천분지구릉구자색토임지토양린소최대흡부량(Qm)급린흡부완충용량(MBC)고우동류형자색토농지토양;임지토양생물유효린함량저우농지;농지린소석방풍험고우임지。상교중성급석회성자색토,산성자색토린소최대흡부량、흡부완충용량저,단린소해흡능력교고,표명산성자색토린소석방풍험교대。다중상관분석표명,진관불동류형자색토pH、유궤질、토양질지등인소대린소흡부해흡병무단일적현저영향,종이무법침대소유3충토양조출기영향린소흡부해흡적공성인소,단인자분석결과표명pH、토양질지급토양총린함량대린소흡부해흡특성잉유직접영향。
Phosphorus is an important limiting nutrient of water eutrophication ,and overdose of farmland phosphate have aggravated the water pollution .In the circumstances of multiple parent materials and land uses ,typical purple soils (Named as Entisol in SAT system ,US) have respectively been collected from forest and farmland in three sites ,representing acidic ,neutral and calcareous soils in hilly area of the Si-chuan Basin .T he characteristics of phosphorus adsorption-desorption of soil samples have been studied by incubation in Lab and Langmuir model analysis methods .Results show that the maximum adsorption ca-pacity (Qm) and buffer capacity (MBC ) of phosphorus ranged from 320 .82 -615 .81 mg/kg ,18 .16 -109 .65 L/kg of forest soils ,and 246 .02-454 .55 mg/kg ,11 .52-69 .30 L/kg of farmland soils ,w hich in-dicates higher phosphorus release risk in farmland .Acidic purple soil has a lower Qm ,MBC and a higher P desorption capacity than neutral and calcareous soil ,w hich indicates that acidic purple soil are easier to lose P than the other two types of purple soil .The multiple regression analysis shows that there are no signifi-cant linear correlations between soil physicochemical properties and the phosphorus adsorption-desorption characteristics ,but factor analysis shows that pH ,organic matter and soil texture have direct impact on soil phosphorus adsorption-desorption ability .