羅 暢 宋國棟 劉素美

羅 暢1, 2, 3宋國棟1, 2①劉素美1, 2

(1. 中國海洋大學(xué) 深海圈層與地球系統(tǒng)前沿科學(xué)中心/海洋化學(xué)理論與工程技術(shù)教育部重點實驗室 山東青島 266100; 2. 青島海洋科學(xué)與技術(shù)試點國家實驗室 海洋生態(tài)與環(huán)境科學(xué)功能實驗室 山東青島 266237; 3. 中國海洋大學(xué)化學(xué)化工學(xué)院 山東青島 266100)

15N加富樣品; 硝化; 氨基磺酸; 膜進樣質(zhì)譜

Tab.1 Some main methods, principles, and characteristics for the determination of 15N labeled

1 材料和方法

1.1 測定15N加富樣品中的分析步驟

圖1 基于鎘柱與氨基磺酸雙還原體系并結(jié)合膜進樣質(zhì)譜測定15N加富樣品中的簡單流程

整個方法涉及多項因素的條件測試, 影響因素和條件設(shè)定如表2, 方法的條件測試具體步驟見1.2～1.5, 方法對樣品的應(yīng)用測試見1.6。

1.2 鎘柱還原率及還原硝酸鹽濃度范圍測定

Tab.2 Influencing factors and conditions for determination of by membrane injection mass spectrometry based on cadmium column and sulfamic acid double reduction (SA) system

1.3 氨基磺酸濃度、試劑酸度及反應(yīng)時間

1.4 線性范圍、精密度及檢測限

檢測限: 以工作曲線線性回歸方程截距標準偏差的3倍除以斜率即檢測限。

1.5 鹽效應(yīng)

1.6 石老人沙灘沉積物中銨氧化與亞硝酸鹽氧化速率的測定

于2019年5月15日早上08:30 (低潮位時刻)在青島石老人沙灘(36°5′48″N, 120°28′25″E)獲取沉積物柱狀樣, 將表層10 cm沉積物以2 cm的垂向分辨率現(xiàn)場進行分割裝入密封袋中; 獲取沉積物的同時獲取5 L海水, 與分割好的沉積物一同保存在裝有冰盒的保溫箱帶回實驗室進行后續(xù)實驗。

2 結(jié)果與討論

2.1 鎘柱還原率

鎘柱還原率≤1, SA還原效率≤1, 為實現(xiàn)轉(zhuǎn)化率越大, 則需和越接近1。

圖2 過柱(a), 過柱(b), 不過柱(c), 過柱與過柱(d)工作曲線

圖3 不同氨基磺酸(SA)濃度(0.5～20 mmol/L)和酸度(HCl濃度0～1 mol/L)條件下, 轉(zhuǎn)化為29N2的信號比值Δ29N2/ΣN2變化(a)和轉(zhuǎn)化率(b)

Fig.3 The signal ratio Δ29N2/ΣN2 variation from to 29N2 (a) and conversion (b) under different sulfamic acid (SA) concentration (0.5～20 mmol/L) and acidity (expressed as HCl concentration 0～1 mol/L)

圖4 10 μmol/L經(jīng)鎘和15 mmol/L SA (1 mol/L HCl)試劑還原后測試信號隨時間的變化

2.3 線性范圍、檢出限和精密度

圖5 鎘柱還原-SA反應(yīng)測定的線性范圍測試

圖6 鎘柱還原-SA反應(yīng)測定的工作曲線(0～10 μmol/L)

Tab.3 Δ29N2/ΣN2 average measured at 1 and 10 μmol/L of standard and the Δ29N2/ΣN2 standard deviation and Δ29N2/ΣN2 relative standard deviation (n = 4)

2.4 鹽效應(yīng)影響

通過測定鹽度范圍為0～35的Δ29N2/ΣN2與鹽度為0時Δ29N2/ΣN2信號比值計算相對誤差(圖7), 表明當(dāng)鹽度為5、30和35, Δ29N2/ΣN2相對誤差明顯低于1%, Δ29N2/ΣN2基本未發(fā)生變化; 當(dāng)鹽度為10～25, Δ29N2/ΣN2相對誤差約為2%, Δ29N2/ΣN2受到的影響也較小。因此, 整個反應(yīng)過程可視為無顯著的鹽效應(yīng)。

圖7 鹽度為0～35時Δ29N2/ΣN2相對誤差變化

2.5 石老人沙灘沉積物中潛在的銨氧化與亞硝酸鹽氧化速率

圖8 加富樣品(a)和加富樣品(b)中生成與培養(yǎng)時間的關(guān)系

Fig.8 Relationship between production and incubation time in -enriched samples (a) and -enriched samples (b)

圖9 氧化為及氧化為的速率與沉積物深度的關(guān)系

3 結(jié)論

致謝 感謝謝成軍同學(xué)對本研究實驗過程與儀器操作所提供的協(xié)助; 感謝廣西大學(xué)海洋學(xué)院寧志銘老師對本文的修改指正。

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LUO Chang1,2,3, SONG Guo-Dong1, 2, LIU Su-Mei1, 2

(1. Frontiers Science Center of Deep Ocean Multispheres and Earth System/Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao 266100, China; 2.Laboratory for Marine Ecology and Environmental Science, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, China; 3. College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China)

15N enriched sample; nitrification; sulfamic acid; membrane injection mass spectrometry

*國家自然科學(xué)基金, U1806211號, 42076035號, 41606093號; 中國海洋大學(xué)中央高?；究蒲袠I(yè)務(wù), 202072001號。羅暢, 碩士研究生, E-mail: 1051392235@qq.com

宋國棟, 副教授, E-mail: gsong@ouc.edu.cn

2021-10-09,

2021-12-02

P734

10.11693/hyhz20211000237