土壤膠質物是存在於土壤中特別的物質,極為細微,具理學成分。膠質此一學術語與晶質有所區別,其亦非食鹽、砂糖等諸溶液的結晶。膠質在土壤中是以物質的形式微量存在的。土壤膠質物的理學性質其一為吸水後的發熱膨脹,更進一步的探討會發現其與水量與土中膠質物之多寡有關,化學性質方面則與土壤中酶基置換作用有關。土壤膠質物與土壤組織結構有很大的影響,對土壤排水、通氣性、可塑性、黏著力諸程度上有相對的影響存在。此外,土壤膠質物亦會影響植物對土壤養分的吸收。 先行研究指出,土壤膠質物的形成與土壤中動植物遺骸及腐植植 ...
長野正
core
[Research progress on poor response, resistance mechanisms, and influencing factors of immunotherapy for hepatocellular carcinoma]. [PDF]
Huang M +5 more
europepmc +1 more source
[Determination of three new herbicide residues in soil, sediment and water by liquid chromatography-tandem mass spectrometry]. [PDF]
He HM +7 more
europepmc +1 more source
[Progress in sample pretreatment and detection methods of hexabromocyclododecanes]. [PDF]
Cheng J, Ma J, Li S, Tian Y.
europepmc +1 more source
[Determination of cycloxaprid and paichongding residues in foods of plant origin by ultra performance liquid chromatography-tandem mass spectrometry]. [PDF]
Liu JJ +9 more
europepmc +1 more source
[Progress in the application of preparative gas chromatography in separating volatile compounds]. [PDF]
Mayira A, Zhong Z, Bai X.
europepmc +1 more source
在分析南亚热带丘陵赤红壤降雨入渗和产流过程基础上 ,依据田间实测资料 ,建立了丘陵赤红壤降雨入渗产流数学模型 ,分析了南亚热带丘陵赤红壤地表径流的动态变化特征及其影响因素。结果表明 ,丘陵赤红壤区 ,4~ 9月每次降雨产生的径流量变化范围为 0 .2~ 5 1.0 4m m,径流率变化范围为 0 .5 6 %~ 47.5 8% ,10月至次年 3月一般不产生地表径流 ;地表径流量与降雨量拟合关系式为 R0 =0 .0 2 5 9.Pn1 .40 34 ,径流率与土壤表层初始含水量拟合关系式为 R′0 ...
doaj
[Design and practice of undergraduate instrumental analysis experiment: analysis of polycyclic aromatic hydrocarbons in environmental water by solid-phase microextraction- liquid chromatography]. [PDF]
Liu J, Wu JY, Li JT, Chen NW, Huang XJ.
europepmc +1 more source
[Application and advances of nanozyme-loaded tissue engineering scaffolds in wound repair]. [PDF]
Hao RN +6 more
europepmc +1 more source
[Research progress of mucormycosis in burns]. [PDF]
Shen T, Zhu F.
europepmc +1 more source

