Skip to main content

ETHNOS_APP

Home • Search • Journals • List 0

Libs and FTIR–ATR spectroscopy studies of mineral–organic associations in saline soil

Bibliographic Data

ID21647747
AuthorsFei Ma (0000-0002-5472-4763, State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences Nanjing PR China), Changwen Du (0000-0002-9064-3581, State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences Nanjing PR China, corresponding author), Yiqiang Zhang (0000-0003-0691-6645, Institute of Water Science Bayannur PR China), Xuebin Xu (0009-0007-5637-6874, State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences Nanjing PR China), Jianmin Zhou (0000-0002-4749-8761, State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences Nanjing PR China)
Year2021
Volume32
Issue4
Pages1786-1795
Publication date2021-02-28
Open AccessYes
TypeARTICLE
VenueLand Degradation and Development (JOURNAL)
Journal identifiersISSN: 1085-3278 • E-ISSN: 1099-145X
PublisherWiley (PUBLISHER • GB)
DOI10.1002/ldr.3829
OpenAlexW3104273122
LanguageEN
References cited30

Direct characterization of the spatial distribution of elements and compound binding of salt–organic associations in soil is imperative for understanding the mechanisms of organic matter decomposition and nutrient release involved in soil degradation and development processes. However, traditional chemical methods would damage the chemical bonds in salt–organic associations, and modern spectroscopic techniques provide alternative options for resolving this problem. In this study, mid‐infrared‐attenuated total reflectance spectroscopy (FTIR–ATR) was used to obtain molecular group information; laser‐induced breakdown spectroscopy (LIBS) was applied to obtain microlevel distribution of elements, and two‐dimensional correlation spectroscopy (2DCOS) analysis was conducted to illustrate the binding combination features of mineral–organic associations in saline soil from the Hetao Irrigation District in China. The results showed that the distributions of Mg, Ca, Na, and K were heterogeneous at the microlevel; the spatial distributions of Mg and Ca showed a significant correlation ( r = 0.90 *** ), while K displayed a negative correlation with the soil organic matter (SOM) contents. In the soil with lower SOM contents, the elements were distributed at the top of the ablation area and enhanced with the increasing SOM content, which reflected the trends of the SOM layer thickness outside the mineral–organic associations at the microlevel. Furthermore, 2DCOS analysis suggested that the hydrogen bonds in silicate groups were stronger than those of organic functional groups, such as C=O/C=C, when combined with salt‐related compounds, and Mg, Ca, Na, and K did not originate from clay mineral compounds in saline soil but partially originated from deposited organic associations

Attenuated total reflection · Decomposition · Fourier transform infrared spectroscopy · Infrared spectroscopy · Organic matter · Soil organic matter · Soil salinity · Soil water · Analytical chemistry methods development · Chemical Engineering · Chemistry · Environmental Science · Heavy metals in environment · Laser-induced spectroscopy and plasma · Environmental Chemistry · Organic Chemistry · Soil Science

  • Smoothing and Differentiation of Data by Simplified Least Squares Procedures.

    Abraham Savitzky, Marcel J E Golay•Analytical Chemistry•1964

  • The contentious nature of soil organic matter

    Open Access•Johannes Lehmann, Markus Kleber•Nature•2015

Highly citedNo

Tools

Open DOI
Ethnos_APP • Open Source Project • MIT License • Frontend v2.0.0 • Privacy and Cookies • API Documentation: api.ethnos.app/docs • API Source Code: GitHub • DOI: 10.5281/zenodo.17049435 • Frontend Source Code: GitHub • DOI: 10.5281/zenodo.17050053 • cruz.rio.br • Expectantes Misericordiae