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基于突變理論的土地質(zhì)量地球化學(xué)評價方法研究
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河北省水資源可持續(xù)利用與產(chǎn)業(yè)結(jié)構(gòu)優(yōu)化協(xié)同創(chuàng)新中心開放基金項目(XTZX202109)和中國地質(zhì)調(diào)查局地質(zhì)調(diào)查項目(DD20179303)


Land Quality Geochemical Evaluation Based on Catastrophe Theory
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    為實現(xiàn)土壤肥力和土壤環(huán)境質(zhì)量相結(jié)合的土地質(zhì)量地球化學(xué)綜合評價結(jié)果的高精度量化,依據(jù)贛南南康地區(qū)采集的6266組表層土壤樣品測試結(jié)果,構(gòu)建了以As、Hg、Cd、Pb、Cr含量等為基礎(chǔ)的內(nèi)梅羅指數(shù)和以有機(jī)質(zhì)(SOM)、P、N、K、Mo、Mn、B、Cu、Zn含量等為基礎(chǔ)的土壤綜合肥力指數(shù)為控制因素的突變理論法土地質(zhì)量地球化學(xué)綜合評價方法,將內(nèi)梅羅指數(shù)3.0修訂為3.1,通過突變理論對數(shù)據(jù)進(jìn)行標(biāo)準(zhǔn)化和歸一化分析,比較原始內(nèi)梅羅指數(shù)和修訂內(nèi)梅羅指數(shù)評價結(jié)果以及本文方法與DZ/T 0295—2016《土地質(zhì)量地球化學(xué)評價規(guī)范》方法的土地質(zhì)量地球化學(xué)綜合等級劃分結(jié)果。結(jié)果表明:研究區(qū)土壤綜合肥力指數(shù)均值為0.75,總體綜合肥力為Ⅲ等,土壤肥力較低;土壤綜合內(nèi)梅羅指數(shù)均值為0.59,總體尚清潔。采用修訂后的內(nèi)梅羅指數(shù)3.1計算的土壤肥力指數(shù)分界值基本呈等級等間距劃分。與DZ/T 0295—2016《土地質(zhì)量地球化學(xué)評價規(guī)范》評價結(jié)果比較,83.57%的結(jié)果等級未發(fā)生變化,近16%等級結(jié)果增加1個等級,主要為1級和2級升為3級和4級,未出現(xiàn)2個及以上等級的變化,評價結(jié)果顯示3級、4級面積占比為94.11%、5.30%。本文方法可用于土地質(zhì)量地球化學(xué)綜合等級評價,評價結(jié)果更加數(shù)值化、精細(xì)化,評價過程更簡便,是對已有土地質(zhì)量地球化學(xué)綜合評價方法的補(bǔ)充,可為土地利用、農(nóng)業(yè)生產(chǎn)和管理提供借鑒和參考。

    Abstract:

    According to the test results of 6266 groups surface soil samples collected in Nankang area of southern Jiangxi, to achieve high-precision quantification of land quality geochemical evaluation coupling soil fertility and soil environmental quality, a cusp catastrophe model was established and applied to evaluate land quality geochemical evaluation. In this model, soil fertility index (Pf), including SOM, P, N, K, Mo, Mn, B, Cu, Zn in solid samples was the main variable, Nemerow index (Pn), including As, Hg, Cd, Pb, Cr in solid samples was the secondary variable, for values greater than 3 of Pf, Pf were revised to 3.1, and the influences of adjusting on the results were compared. The results showed that the average of Pf was 0.75 and the overall level of soil fertility was Ⅲ, the soil fertility was lower, the average of Pn was 0.59 and the overall level of soil contamination was cleaner. The linear relationship between the boundary value of soil fertility index calculated by the adjusting Nemerow index and the land quality grade was better. The results of comparing with DZ/T 0295—2016 showed that 83.57% of the evaluation grades were the same, and nearly 16% of the grade was increased by one grade, the range of grade increase or decrease did not exceed 1. The area of grade 2 was mainly distributed in the southeastern edge and the middle-northern part of the study area, the area of grade 3 was widely distributed, and the area of grade 4 was sporadically distributed. The research results showed that the method can be used for the comprehensive evaluation of land quality geochemistry, with more numerical and simpler evaluation process, it was a supplement to existing methods for comprehensive evaluation of land quality geochemistry which can provide effective reference.

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耿婷婷,劉金巍,宋綿,邊超,曹月婷,劉江濤,張濤.基于突變理論的土地質(zhì)量地球化學(xué)評價方法研究[J].農(nóng)業(yè)機(jī)械學(xué)報,2024,55(8):374-381. GENG Tingting, LIU Jinwei, SONG Mian, BIAN Chao, CAO Yueting, LIU Jiangtao, ZHANG Tao. Land Quality Geochemical Evaluation Based on Catastrophe Theory[J]. Transactions of the Chinese Society for Agricultural Machinery,2024,55(8):374-381.

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  • 收稿日期:2023-11-30
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  • 在線發(fā)布日期: 2024-08-10
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