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土壤磷素化学行为及影响因素研究进展 被引量:76
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作者 刘建玲 张凤华 《河北农业大学学报》 CAS CSCD 北大核心 2000年第3期36-45,共10页
综述了近 42年来关于土壤磷素中化学行为、磷素平衡及影响因素的研究进展。土壤磷素包括无机磷、有机磷、生物态磷 ,土壤无机、有机磷又根据其有效性分为各种形态的无机磷、有机磷组分 ;施入土壤的磷素主要转化为土壤无机磷 ,土壤类型... 综述了近 42年来关于土壤磷素中化学行为、磷素平衡及影响因素的研究进展。土壤磷素包括无机磷、有机磷、生物态磷 ,土壤无机、有机磷又根据其有效性分为各种形态的无机磷、有机磷组分 ;施入土壤的磷素主要转化为土壤无机磷 ,土壤类型、作物种植方式、作物根际、磷肥种类及用量对土壤磷素转化均有不同程度的影响 ;各种高分子有机物料、作物根系分泌有机酸对土壤磷素有明显的活化作用 ;VA菌根真菌明显地促进了作物吸收利用根际、非根际土壤的Ca2 -P ,Ca8-P ,Al-P等形态的无机磷。土壤磷素积累与消耗以无机磷为主 。 展开更多
关键词 土壤磷素形态 磷素转化 磷素平衡 磷肥
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重庆长寿湖富营养化评价及氮磷平衡研究 被引量:24
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作者 杨志敏 熊海灵 +2 位作者 张晟 张可 魏世强 《水土保持学报》 CSCD 北大核心 2005年第2期73-75,109,共4页
利用营养状态卡森指数和综合营养状态指数评价长寿湖富营养状况,结果表明各监测点均达到富营养化水平。长寿湖富营养化主要影响因子氮磷的输入输出研究结果为:氮输入总量7914 6t/a ,主要来源为上游来水,占总量约70 % ;磷输入总量5 91 8... 利用营养状态卡森指数和综合营养状态指数评价长寿湖富营养状况,结果表明各监测点均达到富营养化水平。长寿湖富营养化主要影响因子氮磷的输入输出研究结果为:氮输入总量7914 6t/a ,主要来源为上游来水,占总量约70 % ;磷输入总量5 91 84t/a ,主要来源为农田径流,占总量约4 7% ;氮磷输出量分别为2 4 19 5t/a和12 0 2t/a,截留率分别为6 9 4 %和79 7%。结合该地的实际情况,指出了防止湖泊富营养化加重。 展开更多
关键词 富营养化评价 长寿湖 平衡研究 氮磷 重庆 湖泊富营养化 营养状态 营养状况 指数评价 研究结果 输入输出 影响因子 农田径流 指数和 监测点 输出量 截留率 污染物 龙溪河 上游
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Soil phosphorus dynamic, balance and critical P values in longterm fertilization experiment in Taihu Lake region, China 被引量:16
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作者 SHI Lin-lin SHEN Ming-xing +4 位作者 LU Chang-yin WANG Hai-hou ZHOU Xin-wei JIN Mei-juan WU Tong-dong 《Journal of Integrative Agriculture》 SCIE CAS CSCD 2015年第12期2446-2455,共10页
Phosphorus(P) is an important macronutrient for plant but can also cause potential environmental risk. In this paper, we studied the long-term fertilizer experiment(started 1980) to assess the soil P dynamic, bala... Phosphorus(P) is an important macronutrient for plant but can also cause potential environmental risk. In this paper, we studied the long-term fertilizer experiment(started 1980) to assess the soil P dynamic, balance, critical P value and the crop yield response in Taihu Lake region, China. To avoid the effect of nitrogen(N) and potassium(K), only the following treatments were chosen for subsequent discussion, including: C0(control treatment without any fertilizer or organic manure), CNK treatment(mineral N and K only), CNPK(balanced fertilization with mineral N, P and K), MNK(integrated organic manure and mineral N and K), and MNPK(organic manure plus balanced fertilization). The results revealed that the response of wheat yield was more sensitive than rice, and no significant differences of crop yield had been detected among MNK, CNPK and MNPK until 2013. Dynamic and balance of soil total P(TP) and Olsen-P showed soil TP pool was enlarged significantly over consistent fertilization. However, the diminishing marginal utility of soil Olsen-P was also found, indicating that high-level P application in the present condition could not increase soil Olsen-P contents anymore. Linear-linear and Mitscherlich models were used to estimate the critical value of Olsen-P for crops. The average critical P value for rice and wheat was 3.40 and 4.08 mg kg^(–1), respectively. The smaller critical P value than in uplands indicated a stronger ability of P supply for crops in this paddy soil. We concluded that no more mineral P should be applied in rice-wheat system in Taihu Lake region if soil Olsen-P is higher than the critical P value. The agricultural technique and management referring to activate the plant-available P pool are also considerable, such as integrated use of low-P organic manure with mineral N and K. 展开更多
关键词 long-term fertilization soil p dynamic soil p balance crop yield critical p value
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