[Simultaneous determination of saturated and aromatic hydrocarbons in soil by on-line high performance liquid chromatography-gas chromatography]. [PDF]
Se Pu, 2021 Liu L, Li B, Wu Y.
europepmc +1 more source
Shuitu Baochi Xuebao, 2008 研究土壤水入渗有助于了解喀斯特地区表层岩溶带对降水资源的调蓄作用。该文利用盘式负压入渗仪(盘径d=20 cm,负压h0=-20 mm)研究了桂西北喀斯特洼地典型剖面各层次土壤透水性。结果表明:各层土壤透水性能差异较大,具有随土层深度增加而减小的趋势,但菜地50-80 cm层大于20-50 cm层;菜地剖面0-10 cm层土壤近似饱和导水率(1.85×10-3cm/s)是20-50 cm层的5.2倍,玉米地剖面0-16 cm层土壤近似饱和导水率(2.21×10-3cm/s)是55-70 cm层的3.1倍 ...
LIU, CHEN, ZHANG, SHI
doaj
[Recalling the history of the prevention and treatment during the epidemics of four infectious diseases, including botulism in Xinjiang]. [PDF]
Zhonghua Gan Zang Bing Za Zhi, 2023 Zhao FX, Lu XB, Fu WH, Dilixiati-Yakepu.
europepmc +1 more source
[Simultaneous determination of 30 antibiotics in soil by ultra-high performance liquid chromatography-tandem mass spectrometry]. [PDF]
Se Pu, 2021 Hu Y, Zhu Q, Hu L, Liao C.
europepmc +1 more source
[Research progress on interference in the identification of accelerants in a fire scene]. [PDF]
Se Pu, 2022 Yin G +5 more
europepmc +1 more source
Shuitu Baochi Xuebao, 2016 以江汉平原连续水耕年限大于100 a（老稻田）和由旱耕改为水耕17 a（新稻田）的稻田为研究对象，通过测定土壤剖面基本理化性质和水力学参数，揭示了2种稻田土壤水分渗漏和保持特征差异。结果表明：（1）新稻田土壤的平均饱和导水率（Ks）为32.05 cm/d，显著高于老稻田（17.91 cm/d）。新、老稻田土壤Ks均表现为耕作层＞底土层＞犁底层，新稻田耕作层Ks分别为犁底层和底土层的6.3倍和5.7倍，老稻田耕作层Ks分别是犁底层和底土层的6.9倍和4.0倍。（2）老稻田土壤持水能力高于新稻田 ...
张 +5 more
doaj
[Evaluation of Gradient-Variant Quantum Dot Fluorescence Technology for Rapid Detection of <i>Brucella</i>]. [PDF]
Sichuan Da Xue Xue Bao Yi Xue BanLi J +9 more
europepmc +1 more source
[Applications of molecularly imprinted solid-phase microextraction coupled with chromatography/mass spectrometry for determination of drug residues]. [PDF]
Se PuYan J +8 more
europepmc +1 more source
[Research progress on analytical methods for the determination of hexachlorobutadiene]. [PDF]
Se Pu, 2021 Wang Y, Zhang H, Shi J, Jiang G.
europepmc +1 more source
Shuitu Baochi Xuebao目的为揭示层状土壤剖面的CO2垂直分布规律及其影响因素。方法选取典型层状结构土壤剖面为研究对象，基于土壤剖面构型特征，通过气井法对土壤剖面CO2浓度进行野外监测，并根据菲克定律计算CO2累积通量。结果1）层状结构主导CO2浓度的剖面分布格局。草地土壤中，CO2在剖面不同时期的旋回淤积层中浓度分别为2 449.2、6 201.9、2 736.9、5 284.9 μmol/mol，显示出波动趋势；农地土壤中，CO2在耕层、犁底层、底土层中浓度分别为1 792.3、3 661.4、5 294.7 μmol ...
夏彬, 张佐源, 郝旺林, 许明祥
doaj