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长期施肥下我国典型农田耕层土壤的pH演变 被引量:150
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作者 孟红旗 刘景 +6 位作者 徐明岗 吕家珑 周宝库 彭畅 石孝均 黄庆海 王伯仁 《土壤学报》 CAS CSCD 北大核心 2013年第6期1109-1116,共8页
探索长期不同施肥措施下农田耕层土壤的pH演变,为进一步揭示农田土壤酸化的机制及其预防措施提供依据。收集了我国典型农田6个长期(18~30a)施肥试验(祁阳红壤、进贤红壤、重庆紫色土、公主岭黑土、哈尔滨黑土常量施肥和高量施肥)... 探索长期不同施肥措施下农田耕层土壤的pH演变,为进一步揭示农田土壤酸化的机制及其预防措施提供依据。收集了我国典型农田6个长期(18~30a)施肥试验(祁阳红壤、进贤红壤、重庆紫色土、公主岭黑土、哈尔滨黑土常量施肥和高量施肥)的历史观测资料,对耕层土壤pH在不同试验阶段(每6a)和施肥措施(对照不施肥(CK)、单施化学氮肥(N)、磷钾配施氮肥(NPK)和有机肥配施化肥(NPKM))间的差异性进行检验,并计算土壤酸化速率。结果表明,试验期间,对照CK处理的耕层pH略有降低,平均土壤酸化速率为0.013pHa-1;N处理的1~6a,祁阳红壤、公主岭黑土和哈尔滨黑土常量施肥试验的耕层pH较对照显著降低0.32~0.55个单位,至最近6a,所有试验的耕层pH较对照显著降低0.64~1.46个单位;NPK处理的耕层pH在试验1~12a明显低于N处理;NPKM处理的耕层pH却较NPK处理高0.30~0.53个单位,pH变化趋势与NPK相似。处理间成对T检验表明,长期施肥农田的土壤酸化速率大小顺序为:N〉NPK〉NPKM—CK,N和NPK处理的土壤酸化速率分别为对照的4.6倍和3.2倍。基于湿润或半湿润地区排水良好的旱作或水旱轮作农田分析了农田土壤酸化过程。尽管存在地域差异性,长期施肥农田耕层土壤的pH演变存在对施肥措施的共性响应特征。 展开更多
关键词 土壤酸化 ph演变 长期施肥 共性响应 地域差异性
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pH值演变对果蔬垃圾厌氧发酵效能的影响研究 被引量:2
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作者 石川 刘越 +3 位作者 罗娟 吴厚凯 王凯军 周岳溪 《中国沼气》 2022年第2期3-10,共8页
果蔬垃圾的高效转化和循环利用对解决环境污染、能源匮乏和资源紧缺等问题具有正向作用。以果蔬垃圾为发酵底物,厌氧污泥作为微生物接种物,通过半连续实验对比不调节pH值和调节pH值(2.0~12.0)厌氧体系的发酵组分,考察不同pH值发酵体系... 果蔬垃圾的高效转化和循环利用对解决环境污染、能源匮乏和资源紧缺等问题具有正向作用。以果蔬垃圾为发酵底物,厌氧污泥作为微生物接种物,通过半连续实验对比不调节pH值和调节pH值(2.0~12.0)厌氧体系的发酵组分,考察不同pH值发酵体系的水解酸化效率、产物组分、营养元素释放及微生物能量情况,以反映pH值生态因子对果蔬垃圾厌氧发酵效能的持续影响。结果表明,果蔬垃圾厌氧自然酸化发酵pH值维持在3.0~5.0,优势产物为乳酸,产量可达9198.54 mg·L^(-1)。相比自然酸化发酵,pH值调控下的厌氧发酵产量提高,且在酸碱条件下呈现不同的发酵类型。酸性条件下,优势产物为乳酸和乙醇,占酸化产物比例可达59.97%和78.13%。碱性条件下,乙酸、丙酸和丁酸为主要厌氧酸化产物,其组分最高分别可达87.71%,20.25%和35.87%。碱性条件下,厌氧水解率和酸化率普遍偏高,分别为84.94%和75.18%。但酸性发酵液中富含更多NH_(4)^(+)-N和PO_(4)^(3-),分别高达1180.13 mg·L^(-1)和477.70 mg·L^(-1)。微生物能量水平与酸化产物总量具有负相关性。酸性和碱性pH值演变对果蔬垃圾厌氧发酵组分和效能具有关键调控作用。 展开更多
关键词 ph演变 厌氧发酵 果蔬垃圾 脂肪酸 氮磷营养
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Ammonium Variational Trends and the Ammonia Neutralization Effect on Acid Rain over East Asia
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作者 GAO Chao WANG Zi-Fa Enagnon A. GBAGUIDI 《Atmospheric and Oceanic Science Letters》 2010年第2期120-126,共7页
The distribution and variations of ammonium and the ammonia neutralization effect on acid rain were examined in East Asia during the period of 2000 05 using observed wet deposition data from the Acid Deposition Monito... The distribution and variations of ammonium and the ammonia neutralization effect on acid rain were examined in East Asia during the period of 2000 05 using observed wet deposition data from the Acid Deposition Monitoring Network in East Asia (EANET).Observational trends show a high proportion of NH 4 + in the total cations,with a six-year mean proportion of over 20% for continental and inland regions.The concentrations and deposition of NH 4 + were higher in western China and Vietnam than in other regions.The annual variations in NH 4 + concentration were smooth in most of the regions,except for southern China and Vietnam,where the NH 4 + concentrations increased,and western China,where the NH 4 + concentrations decreased.The neutralization factors (NFs) of NH 4 + indicate that ammonia has a great neutralization capability toward acid rain,including for the regions with low NH 4 + concentrations,such as Japan.The NFs were high in summer,with no obvious discrepancies between the northern and southern stations.However,the correlation coefficients between NH 4 + concentrations and rain pH values imply that the ammonia neutralization effects on the pH values were distinct only at southern China and southern Japan stations.The neutralization of precipitation by ammonia was estimated by comparing the discrepancies between the observed pH values and the pH values calculated without ammonia consuming the H + in NH 4 +.The results demonstrate that ammonia may increase annual mean pH values by 0.4 0.7 in southern China and by 0.15 0.25 in southern Japan. 展开更多
关键词 acid rain AMMONIUM neutralization effect
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