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[1]FangshiJiang,PengyuGao,XiaojingSi,ZhenzhiZhan,HaidongZhang,JinshiLin,XiangJi,MingKuangWang,YanheHuangModellingthesedimenttransportcapacityofflowsinnon-erodiblerills[J].Hydrologicalprocesses,2018,32:3852–3865
[2]Jiang,F.S.,Huang,Y.H.,Wang,M.K.,Lin,J.S.,Ge,H.L.&Ji,X.Rillerosionprocessesonasteepcolluvialdepositslopeunderheavyrainfallinflumeexperimentswithartificialrain[J].Catena,2018,169,45–58.
[3]Jiang,F.S.,Huang,Y.H.,Wang,M.K.,Lin,J.S.,Ge,H.L.&Ji,X.SedimentselectivebehaviorsofcolluvialdepositmaterialsonsteepslopesandunderheavyrainfallconditionsinsoutheasternChina[J].JournalofSoilandWaterConservation,2018,73,156–165.
[4]Fang-shiJiang,Yan-heHuang,Ming-kuangWang,Jin-shiLin,GanZhao,Hong-liGe.EffectsofRainfallIntensityandSlopeGradientonSteepColluvialDepositErosioninSoutheastChina[J].SoilScienceSocietyAmericaJournal.2014,78(5):1741-1752(封面).
[5]XiangJi,AnitaThompson,JinshiLin,FangshiJiang,ShaoxinLi,MingmingYu,YanheHuang*.Simulatingandassessingtheevolutionofcollapsinggulliesbasedoncellularautomata-Markovandlandscapepatternmetrics:acasestudyinSouthernChina.JournalofSoilsandSediments,2/25/2019.
[6]Chen,J.L.,Zhou,M.,Lin,J.S.,Jiang,F.S.,Huang,B.F.,Xu,T.T.,Wang,M.K.,Ge,H.L.,&HuangY.H..Comparisonofsoilphysicochemicalpropertiesandmineralogicalcompositionsbetweennoncollapsiblesoilsandcollapsedgullies[J].Geoderma,2018,317,56-66.
[7]Lin,J.S.,Huang,Y.H.,Zhao,G.,Jiang,F.S.,Wang,M.K.,&Ge,H.L..Flow-drivensoilerosionprocessesandthesizeselectivityoferodedsedimentonsteepslopesusingcolluvialdepositsinapermanentgully[J].Catena,2017,157,47–57.
[8]Lin,JS;Zhu,GL;Wei,J;Jiang,FS;Wang,MK;Huang,YH.Mulchingeffectsonerosionfromsteepslopesandsedimentparticlesizedistributionsofgullycolluvialdeposits[J].Catena,2018,160,57–67.
[9]JLin,YHuang,MWang,FJiang,XZhang,HGe.Assessingthesourcesofsedimenttransportedingullysystemsusingafingerprintingapproach:AnexamplefromSouth-eastChina[J].Catena,2015,129:9-17.
[10]蒋芳市,何恺文,李慧,林根根,彭绍云,岳辉,林金石,黄炎和.2种草本植物根系对崩岗洪积扇土壤分离的影响[J].水土保持学报,2018,32(06):112-117.
[11]蒋芳市,陈培济,黄炎和,等.集中水流下土石混合物崩积体坡面侵蚀水动力特征试验研究[J].水土保持学报,2017,31(6):8–14.
[12]蒋芳市,黄炎和*,林金石,赵淦,葛宏力,林敬兰.不同结皮条件对崩岗崩积体坡面侵蚀的影响[J].水土保持学报,2014,28(3):1-6.
[13]蒋芳市,黄炎和*,林金石,赵淦,葛宏力,林敬兰.坡度和雨强对崩岗崩积体侵蚀泥沙颗粒特征的影响[J].土壤学报,2014,51(5):974-982.
[14]蒋芳市,黄炎和*,林金石,赵淦,葛宏力.多场次降雨的崩岗崩积体细沟侵蚀的影响[J].中国水土保持科学,2014,51(5):1-6.
[15]蒋芳市,黄炎和*,林金石,赵淦,葛宏力.花岗岩崩岗崩积体颗粒组成及分形特征[J].水土保持研究,2014,21(6):175-180.
[16]蒋芳市,黄炎和*,林金石,赵淦,葛宏力.坡度和雨强对花岗岩崩岗崩积体细沟侵蚀的影响[J].水土保持研究,2014,21[J]:1-4.
[17]蒋芳市,黄炎和*,林金石,赵淦,张燕,庄雅婷,葛宏力,林敬兰.崩岗崩积体土壤渗透特性分析[J].水土保持学报,2013,27(3):49-54.
[18]蒋芳市,黄炎和*,林金石,赵淦,林浠,赵淦,张燕,谢小芳,扶恒.坡面水流分离崩岗崩积体土壤的动力学特征[J].水土保持学报,2013,27(1):86-89+229.